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"subarctic" Definitions
  1. relating to the region just south of the Arctic Circle
"subarctic" Synonyms
boreal northern septentrional

1000 Sentences With "subarctic"

How to use subarctic in a sentence? Find typical usage patterns (collocations)/phrases/context for "subarctic" and check conjugation/comparative form for "subarctic". Mastering all the usages of "subarctic" from sentence examples published by news publications.

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Eurasian woodcocks are birds native to temperate and subarctic Eurasia. 
However, there is much more to the subarctic region than just the climate.
The bear cams will be watching, with some 18 hours of subarctic daylight.
Researchers sampled barite, a mineral more than 2 billion years old, in subarctic Canada's Belcher Islands.
The temperatures during these drives reached lows of -18F, which is cold even by my subarctic Canadian standards.
Few places on the planet offer a more dramatic juxtaposition of extremes: the climate ranges from desert to subarctic conditions.
The city is often referred to as "China's Arctic town," and is one of the few locations in China to have a subarctic climate.
The subarctic town, nicknamed "Paris of the North" during the late 19th-century Gold Rush, looked like a strange, solitary incursion on the land.
She works in Nain Nunatsiavut, a small Inuit town in Newfoundland and Labrador, and walks to work in subarctic temperatures, or takes a Ski-Doo.
Most of that population is in Whitehorse, leaving the bulk of the territory uninhabited, a subarctic landscape of tundra and mountains stretching north toward the pole.
Her work largely focuses on social justice and inequality, and her reporting has taken her all over — from across the US to India to the Subarctic.
WINNIPEG, Manitoba/OTTAWA (Reuters) - After failing to grow wheat in Canada's subarctic Yukon territory 2000 years ago, farmer Steve Mackenzie-Grieve gave it another shot in 24.3.
This famous recluse once took a five-month trip around the world as well as a subarctic train expedition, both times traveling with just her camera for company.
WINNIPEG, Manitoba/OTTAWA, March 22 (Reuters) - After failing to grow wheat in Canada's subarctic Yukon territory 2000 years ago, farmer Steve Mackenzie-Grieve gave it another shot in 24.3.
This year, I reported from the subarctic village, where, crossing sea ice by snowmobile with a hunter, I learned about this majestic, unforgiving landscape, which is changing at a disorienting rate.
On a sunny May morning in 2014, as the Alaskan subarctic was beginning to warm up, park rangers watched a young female bear, Tundra, explore the marshland around the famous Brooks River.
But have you heard this special species of deer, called caribou in North America and native to Arctic and subarctic regions, is considered "vulnerable" by the International Union for Conservation of Nature (IUCN) Redlist?
By x-ray scanning that skull and carefully analyzing a digital model, paleontologists have now determined that it belongs to an extinct river dolphin that swam in subarctic marine waters some 25 million years ago.
Both bears — voted upon by the public on Katmai National Park's Facebook page — are unquestionably victors in their wild bear world, an Alaskan subarctic environment where snow has already fallen, and the winter looms large.
Reindeer belong in Arctic and subarctic regions, where they can roam freely over vast open ranges, but most of those in captivity are held inside tiny sheds, put on public display and used for photo ops.
The arctic and subarctic ecosystems of the region have evolved to rely on these floods, and scientists are very concerned about what this could mean for the environment, says Berit Arheimer, an author on the study from the Swedish Meteorological and Hydrological Institute.
The installation includes recordings Mr. Krause made in Algonquin Park in Ontario, where he found himself caught between two packs of wolves; in the Yukon Delta, a subarctic area in Alaska, where birds from different continents converge; and in the Central African Republic, where he heard monkeys.
CreditCreditAndy Haslam for The New York Times Last fall, just a few days into my trip to the Shetland Islands, the Scottish subarctic archipelago across the sea from Norway, I found myself on the top of a cliff face, peering through the fog at a huge rock in the northern Atlantic Ocean.
Steppe Climate. Retrieved on 2008-04-15. A subarctic climate has little precipitation,Michael Ritter. Subarctic Climate.
Arkhangelsk experiences a subarctic climate (Köppen climate classification Dfc), with long (November–March) and very cold winters and short (June–August) and cool summers. Arkhangelsk is the largest city in the world with a subarctic climate. Much of Western Calgary in Canada experiences a subarctic climate, and has a much larger population, but not all of the city has a subarctic climate so it doesn't count. Krasnoyarsk in Siberia also has a borderline subarctic climate with the suburbs and northern parts of the city experiencing a subarctic climate and has a population over 1 million, but the whole city doesn't experience a subarctic climate so it also doesn't count.
"Influence of short-term low temperature on net photosynthesis in some subarctic lichens." Reports of the Kevo Subarctic Research Station 8:63-72.
Map of sub-arctic regions Indigenous peoples of the Subarctic are the aboriginal peoples who live in the Subarctic regions of the Americas, Asia and Europe, located south of the true Arctic. This region includes the interior of Alaska, the Western Subarctic or western Canadian Shield and Mackenzie River drainage area, the Eastern Subarctic or Eastern Canadian Shield, Scandinavia, Western Russia and East Asia."Native Art." The Canadian Encyclopedia.
The surrounding area of Moosonees Lake is part of the subarctic climate zone. The vegetation around the lake consists of mainly sparse and often low-growth subarctic woods.
Helm, June. (1981). Handbook of North American Indians: Subarctic. Smithsonian Institution The total inventory of phonemes present in Tagish includes:McClellan, C. (1978). Tagish. In Handbook of North American Indians: Subarctic (Vol.
According to the Köppen-Geiger climate classification system, Kedarnath's climate is monsoon- influenced subarctic climate (Dwc), bordering a uniform rainfall subarctic climate (Dfc) with mild, rainy summers and cold, snowy winters.
Gustavus has a wet, maritime subarctic climate (Köppen Dfc).
Port Alsworth has a continental subarctic climate (Köppen Dfc).
Chersky has a subarctic climate (Köppen climate classification Dfc).
Kananaskis experiences a subarctic climate (Köppen climate classification Dfc).
Kotlas has a subarctic climate (Köppen climate classification Dfc).
Ennadai has a subarctic climate (Köppen climate classification Dfc).
Wabasca has a subarctic climate (Köppen climate classification Dfc).
Kananaskis experiences a subarctic climate (Köppen climate classification Dfc).
Onega has a subarctic climate (Köppen climate classification Dfc).
Aishihik has a subarctic climate (Köppen climate classification Dfc).
Dry Creek has a subarctic climate (Köppen climate classification: Dfc).
Northway has a dry- winter continental subarctic climate (Köppen Dwc).
Tanacross has a dry-winter continental subarctic climate (Köppen Dwc).
Hope has a dry-summer continental subarctic climate (Köppen Dsc).
Salcha has a dry-winter continental subarctic climate (Köppen Dwc).
Livengood has a dry-winter continental subarctic climate (Köppen Dwc).
Manley Hot Springs has a continental subarctic climate (Köppen Dfc).
Circle Hot Springs has a continental subarctic climate (Köppen Dfc).
McGill University operates the McGill Subarctic Research Station in Schefferville.
Berthoud Pass has an extreme alpine subarctic climate (Köppen Dfc).
Native subarctic peoples have over 38 languages into nine major language families: Algonquian,Corbett, Steve. "Native Peoples of the Subarctic." Johnson County Community College. (retrieved 21 Nov 2010) Athapaskan, Indo-European, Turkic and Uralic.
Moose Pass has a dry-summer continental subarctic climate (Köppen Dsc).
Kyusyur has a slightly strong subarctic climate (Dfc borders on Dfd).
Sils-Segl Maria features a cold subarctic climate (Dfc) on Köppen classification.
Usolye- Sibirskoye has a dry-winter subarctic climate (Köppen climate classification: Dwc).
Willow has a subarctic climate with long and cold winters and mild summers.
The area has a subarctic climate (Dfc) bordering on a tundra climate (ET).
Nyurba has an extremely cold dry-summer subarctic climate (Köppen climate classification: Dsc).
According to the Köppen-Geiger system, Hikkim's climate is a subarctic climate (Dfc).
According to the Köppen climate classification system, Warren has a subarctic climate (Köppen Dfc).
McCarthy has a dry-summer subarctic climate (Köppen climate classification: Dsc), similar to Anchorage.
Sandy Lake has a subarctic climate (Dfc) with severely cold winters and mild summers.
Kandalaksha has a subarctic climate (Dfc) with mild, rainy summers, and cold, snowy winters.
Coleman has a subarctic climate (Dfc) with mild to warm summers and cold, snowy winters.
Iliamna has a continental subarctic climate (Köppen Dfc) with mild summers and severely cold winters.
Sutton has a continental subarctic climate (Köppen Dfc) with cold, snowy winters and mild summers.
Mekoryuk has a tundra climate (Köppen: ET), that borders on a subarctic climate (Köppen: Dfc).
Dillingham has a typical subarctic climate (Köppen climate classification: Dfc), relatively average by Alaskan standards.
The southernmost parts of the country are almost tropical, while the northernmost part is subarctic.
Omsukchan has a subarctic climate, with average temperatures ranging from in January to in July.
The Köppen climate classification classifies the climate here as subarctic, and abbreviates this as Dfc.
Fort Hope has a subarctic climate (Dfc) with long, cold winters and short, rainy summers.
Red Dog Mine has a subarctic climate (Dfc) with mild summers and severely cold winters.
Ndilǫ has a subarctic climate (Dfc) with mild to warm summers and long cold winters.
Shoyna has a subarctic climate (Dfc) with short, moderately warm summers and long, cold winters.
Syngrapha diasema is a moth of the family Noctuidae. It is found from northern Fennoscandia to Siberia, across the Arctic and subarctic. In North America, it has been reported across the arctic and subarctic from Labrador to Central Alaska. The wingspan is 30–33 mm.
Samjiyon has a subarctic climate (Köppen climate classification Dwc) with cool summers and cold, dry winters.
Khandud has a subarctic climate (Köppen climate classification Dsc) cold, snowy winters with and cool summers.
Ross River has subarctic climate (Dfc) with long, severely cold winters and short but mild summers.
Lazy Mountain has a continental subarctic climate (Köppen Dfc) with cold, snowy winters and mild summers.
Chesterfield Inlet has a subarctic climate (Dfc) with short but cool summers and long cold winters.
Dixie has a dry summer continental subarctic climate (Dsc) according to the Köppen climate classification system.
Coenagrion interrogatum, the Subarctic bluet, is a blue and black, pond damsel of the family Coenagrionidae.
Carmacks has a subarctic climate (Dfc) with short but mild summers and long, severely cold winters.
Chandalar has a continental subarctic climate (Köppen Dfc). The nearest weather station is at Chandalar Lake.
Wollaston Lake has a subarctic climate (Dfc) with mild, wet summers and long, severely cold winters.
Kobuk has a typical subarctic climate (Köppen climate classification: Dfc), bordering on a dry-winter subarctic climate (Köppen climate classification: Dwc). Kobuk is located at (66.917579, -156.906829). Kobuk is located on the bank of the Kobuk River, northeast of Shungnak. It is near Kobuk Valley National Park.
The predominant climate in the Ardahan province is humid continental climate (Köppen climate classification Dfb) bordering on a subarctic climate (Dfc), with most large settlements in the province being located in lowest possible elevation areas, in attempt to avoid the year-round cold temperatures, thus staying just below the subarctic limit. Smaller locales, districts, villages and a significant portion of the landscape, exhibits a true subarctic climate (Dfc), being the second most widespread climate in the region.
Global map of the subarctic region The subarctic zone is a region in the Northern Hemisphere immediately south of the true Arctic and covering much of Alaska, Canada, Iceland, the north of Scandinavia, Siberia, the Shetland Islands, and the Cairngorms. Generally, subarctic regions fall between 50°N and 70°N latitude, depending on local climates. Precipitation is low, and vegetation is characteristic of the taiga. Daylight at these latitudes are quite extreme between summer and winter.
This ash and iron deposition resulted in one of the largest phytoplankton blooms observed in the subarctic.
Northern Athapaskan Languages. Handbook of North American Indians, Vol. 6: Subarctic, ed. by June Helm, 67–85.
Erdenemandal experiences a subarctic climate (Köppen Dwc) with long, dry, very cold winters and short, warm summers.
A more typical subarctic climate, like Oymyakon, Russia has a temperature lag of only about 15 days.
Eckville experiences a humid continental climate (Köppen climate classification Dfb) which borders on a subarctic climate (Dfc).
A.M. Prokhorov . - 3rd ed. - M, 1969-1978. The climate prevailing in the Vilyuy Plateau is subarctic continental.
The Subarctic Frontal Zone or Subarctic Boundary, about 42⁰N, is fixed in the North Pacific Current. The Subarctic Frontal Zone, slightly south of the maximum westerly wind speeds, separates the North Pacific Subpolar Gyre from the Subtropical Gyre. In the central and eastern Pacific at roughly 32⁰N is the Subtropical Frontal Zone. Sometimes referred to as the Subtropical Convergence Zone, this frontal zone serves as the boundary between the west flowing North Equatorial Current from the North Pacific Current.
Ice Mountain's ice vents provide a habitat for boreal species of plants commonly found in Subarctic regions. The ecosystem exhibits a combination of Appalachian, Canadian, and Subarctic species in a humid subtropical climate. Northern boreal species have survived at Ice Mountain since the last glacial period and became isolated over time as temperatures warmed and relegated the boreal species to the Subarctic regions of North America. The cool air expulsed by the ice vents allowed boreal species to remain at Ice Mountain.
Mogocha has a subarctic climate (Köppen climate classification Dwc) with bitterly cold, dry winters and mild, rainy summers.
Okhotsky-Perevoz has an extreme subarctic climate (Köppen Dfd) with extremely cold, long winters, and short, damp summers.
Ossora has a subarctic climate (Köppen: Dfc), The hottest month is July , and the coldest month is January .
Buy has a cold humid continental climate that is just above subarctic, courtesy of May being just above .
Angustibacter luteus is a bacterium from the genus of Angustibacter which has been isolated from subarctic forest soil.
Pokrovskoye has a typical southern Siberian humid continental climate (Köppen: Dfb), bordering on a subarctic climate (Köppen: Dfc).
Beaverlodge experiences a subarctic climate (Köppen climate classification Dfc) that borders on a humid continental climate (Köppen Dfb).
Okhotsk has a subarctic climate (Köppen climate classification Dwc) with very cold, dry winters and mild, wet summers.
Tungsten has a subarctic climate (Dfc) with long, severely cold winters and short but mild and rainy summers.
Ust-Yudoma has an extreme subarctic climate (Köppen climate classification: Dfd) with extremely cold winters and warm summers.
The vegetation is sparse and consists mostly of low subarctic woodland. The fell is in the subarctic climate zone with a mean annual temperature of -4 °C. The warmest month is July with an average temperature of 14 °C, the coldest is February with a mean temperature of -18 °C.
Ekimchan has a subarctic climate (Köppen climate classification Dwc) with dry and bitterly cold winters and warm, wet summers.
The airport is placed in the permafrost zone with a subarctic climate. The cold season lasts about 8 months.
Teller has a continental subarctic climate (Köppen Dfc), although its climate nearly qualifies as a tundra climate (Köppen ET).
Nederland has an alpine subarctic climate (Dfc) due to its high altitude, with warm summers and long cold winters.
Fitzgerald has a subarctic climate (Köppen climate classification Dfc). Summers are short and warm, and winters long and cold.
Burgeo has a subarctic climate (Dfc) with long, cold winters and short, cool summers. Precipitation is heavy year round.
Cassiar has a subarctic climate (Köppen climate classification Dfc) with long, cold, and snowy winters and short, cool summers.
Ribbed bog moss occurs in arctic, subarctic, boreal, and subboreal zones with cold meso-thermal, oceanic, continental, or cold-humid climates. It is more common in arctic, subarctic, and boreal than subboreal zones. A survey of bryophytes on peatlands across Alberta's Mackenzie River basin found optimal ribbed bog moss growth occurred on sites with annual temperatures ranging from 20 to 32 °F (-4 to 0 °C). In interior arctic, subarctic, and boreal zones, climate is strongly continental in the west, becoming more humid to the east.
Zhigansk has a regular extreme subarctic climate (Köppen climate classification: Dfd), though despite its extreme subarctic climate classification, the town is not quite as cold in winter as some towns with a similar climate, such as Verkhoyansk or Oymyakon, both of which are located further east, in valleys and with no ocean moderation whatsoever. Despite its Dfd classification, precipitation is somewhat higher in summer than at other times of the year, but like other extreme subarctic climates, its precipitation remains rather low year-round.
Burwash Landing has a typical subarctic climate (Köppen climate classification Dfc), bordering on a dry-winter subarctic climate (Köppen climate classification Dwc). Burwash Landing holds the record for the warmest temperature ever recorded in the Yukon in January at . The previous Yukon record of , was set in Whitehorse on January 13, 2013.
Bomnak has a dry- winter subarctic climate (Köppen climate classification Dwc) with dry, bitterly cold winters and warm, wet summers.
July is also generally the wettest month, with an average precipitation of about . This corresponds to a continental subarctic climate.
Batamai has an extreme subarctic climate. (Köppen Dfd, bordering on Dwd) with extremely cold, long winters and short, warm summers.
Under the Köppen climate classification, Churchill Falls has a subarctic climate (Dfc) with long, cold winters and short, mild summers.
Vayda-Guba has a subarctic climate (Dfc) with cool, wet summers and very cold winters lasting most of the year.
Tynda has a subarctic climate (Köppen climate classification Dwc) with severely cold, rather dry winters and warm, very rainy summers.
Native conifer forest communities are located in the highlands. The forest types are mainly subarctic (boreal) and cool-temperate forest.
Trichinella nativa is a nematode worm, one of the species of the genus Trichinella, found in arctic and subarctic regions.
Most subarctic climates have little precipitation, typically no more than over an entire year. Away from the coasts, precipitation occurs mostly in the warmer months, while in coastal areas with subarctic climates the heaviest precipitation is usually during the autumn months when the relative warmth of sea vis-à-vis land is greatest. Low precipitation, by the standards of more temperate regions with longer summers and warmer winters, is typically sufficient in view of the very low evapotranspiration to allow a water-logged terrain in many areas of subarctic climate and to permit snow cover during winter. A notable exception to this pattern is that subarctic climates occurring at high altitudes in otherwise temperate regions have extremely high precipitation due to orographic lift.
From the west climates vary from maritime and maritime subarctic climates. In the north and central climates are generally subarctic or Arctic and to the east climates are mostly subarctic and temperate/continental. Just as both climate and relief are variable across the region, so too is vegetation, with sparse tundra in the north and high mountains, boreal forest on the north-eastern and central regions temperate coniferous forests (formerly of which a majority was in the Scottish Highlands and south west Norway) and temperate broadleaf forests growing in the south, west and temperate east.
Ust-Nera has an extremely cold subarctic climate (Köppen climate classification Dwd) with mild, wet summers and severely cold, dry winters.
Due to its high elevation, Cora experiences a subarctic climate (Köppen Dfc) with long, cold, dry winters and short, cool summers.
Nizhny-Bestyakh has a strong subarctic climate (Köppen Dfd). However summer can be quite warm, sometimes exceeding 30 °C (86 °F).
Alto Río Senguer has a mediterran influenced subarctic climate (Dsc) with short, moderately warm, dry summers and cold, somewhat snowy winters.
Whiteface Mountain has a subarctic climate (Dfc) according to the Köppen climate classification, with very cold, snowy winters and mild summers.
Taymylyr lies on the July 10°C isotherm and has a tundra climate (ET) closely bordering on a subarctic climate (Dfc).
Chokurdakh has an extreme subarctic climate (Dfc), bordering on polar. Temperatures have never risen above zero from November through to March.
Timrå has historically had a subarctic climate, but it has in recent decades more resembled a cool-summer humid continental climate.
2) Subarctic With Cool Summers And Dry Winters (Dwc). Dwc climates are characterized by their coldest month averaging below 0 °C (32 °F), 1–3 months averaging above 10 °C (50 °F), and 70% or more of average annual precipitation received in the warmest six months. 3) Subarctic With Cool Summers And Year Around Rainfall (Dfc).
The climate of Western Alaska is determined largely by the Bering Sea and the Gulf of Alaska. It is a subarctic oceanic climate in the southwest and a continental subarctic climate farther north. The temperature is somewhat moderate considering how far north the area is. This area has a tremendous amount of variety, especially when considering precipitation.
Rankin Inlet has a subarctic climate (Köppen climate classification Dfc), just short of a tundra climate. It is above the tree line. Temperatures stay below freezing from late September to early June. Although the climate is subarctic, temperatures rise and fall too rapidly and do not stay above for long enough (30 days) for trees to grow.
Kelly has a humid continental climate (Dfb) bordering on a subarctic climate (Dfc) with warm to hot summers and very cold winters.
Platinum has a subarctic climate (Dfc) with short, cool and rainy summers and long, cold winters with moderate snowfall peaking during March.
Chamdo has a humid continental climate (Köppen: Dwb) in the Karub District and an alpine subarctic climate (Köppen: Dwc) in other counties.
Chita experiences a dry-winter subarctic climate (Köppen climate classification: Dwc) with very cold, very dry winters and warm, relatively wet summers.
Sunderland, Mitchell (January 3, 2015). Life as a Stripper in a Subarctic Indoor Mining Town. Vice Media, LLC. Retrieved June 14, 2015.
Subarctic Medial LLC. KTOE aired a full service AC format during the 1980s and was once an affiliate of American Top 40.
Based on the Köppen climate classification, Mount Worthington is located in a subarctic climate with long, cold, snowy winters, and mild summers.
Lynn Lake experiences a subarctic climate (Köppen Dfc) with severely cold and long winters and short, mild sometimes warm and rainy summers.
Hatch, Scott A.; Hatch, Martha A. (1990-08-01). "Breeding seasons of oceanic birds in a subarctic colony". Canadian Journal of Zoology.
Hemiboreal means halfway between the temperate and subarctic (or boreal) zones. The term is most frequently used in the context of ecosystems.
Based on the Köppen climate classification, Mount Maxwell is located in a subarctic climate with long, cold, snowy winters, and mild summers.
Kyra has a borderline subarctic/humid continental climate (Köppen climate classification Dwc/Dwb) with very dry, severely cold winters and warm, wet summers.
Nikolaevsk features a subarctic climate (Köppen: Dfc) with short, quite mild summers and long, cold winters. The place experiences a significant marine influence.
Due to high elevation, Toora-Khem has a subarctic climate (Köppen climate classification Dwc) with bitterly cold, long winters and mild, damp summers.
Rena has a subarctic climate (Dfc) although it has some of the warmest summer days in Norway. Winters are very cold and snowy.
Tourism in recent years has become a major source of revenue for most countries of the subarctic due to the beautiful, generally glacial, landscapes so characteristic of the region. Most areas in the subarctic are among the most expensive places in the world to visit, due to both high costs of living and inaccessibility. Nonetheless, the great opportunities for outdoor recreation lure an ever-increasing number of travelers. At the same time, the older industries of the subarctic (fishing, mining, hydroelectric power) are being threatened by both environmental opposition and overfishing leading to depleted stocks of commercially important species.
It being a subarctic climate is a result of the low September night temperatures. Given that Gustavsfors is located somewhat north and Hagfors being a little bit more urban, it is quite possible that the locality just reaches the continental threshold that would require September mean temperatures. In terms of the official reference period of 1961-1990 however, the area is firmly subarctic.
Considering it being at the subarctic threshold and inland, winters are, on average, quite mild for the classification, as is the annual mean temperature.
Most areas of the Kola Peninsula are subarctic climate (Köppen climate classification: Dfc). The nearby islands usually belong to tundra (Köppen climate classification: ET).
The climate in Pampa Alta Pass is subarctic (Csc/Dsc, according to the Köppen climate classification), with drier summers than winters and frequent snowfalls.
Tana has a subarctic climate (Dfc) typical of Northern Norway with long, cold winters lasting most of the year and short, but cool summers.
Most areas of the Kola Peninsula are subarctic climate (Köppen climate classification: Dfc). The nearby islands usually belong to tundra (Köppen climate classification: ET).
Subarctic climate, with an average annual temperature of 0,3C. For the period 1931-1970 the lowest recorded temperature was -27,4C, while the highest - +22,7C.
Cape Alevina has a transitional arctic tundra/subarctic climate (Köppen climate classification ET/Dfc) with very cold, long winters and short, rather cool summers.
Ostrovnoye has a subarctic climate (Koppen Dfc) McKnight and Hess, pp.232-5 with very cold, dry winters, and very mild, somewhat wetter summers.
Chisasibi has a subarctic climate (Köppen Dfc), typical of the central latitudes of Quebec, with very cold and snowy winters and mild, rainy summers.
Peatlands insulate the permafrost in subarctic regions, thus delaying or preventing thawing of permafrost during summer, as well as inducing the formation of permafrost.
The subarctic climate and barrenlands terrain support barren-ground caribou, grizzly bear, muskoxen, Arctic hare, and Arctic fox. The lake's fish include searun Arctic char.
Vayegi has a subarctic or boreal (taiga) climate (Dfc)McKnight and Hess, pp. 232–235 with bitterly cold, very long winters and short, mild summers.
Tavayvaam has a subarctic taiga climate (Koppen climate classification Dfc).McKnight and Hess, pp. 232-235 with very cold, long winters and short, mild summers.
Serevodvinsk has a subarctic climate (Köppen climate classification Dfc) with mild summers with cool nights and long, cold winters. Precipitation is very common year round.
Kirkwood has a dry-summer subarctic climate (Köppen climate classification: Dsc). Summertime is very mild, with little precipitation, while winter is very wet and cold.
Cypress Mountain has a subarctic climate (Köppen Dfc) using the 0 ˚C isotherm and a subpolar oceanic climate (Köppen Cfc) using the -3 ˚C isotherm.
Silverton has an alpine subarctic climate (Köppen climate classification Dfc) with very cold, snowy winters and cool to warm summers with adequate precipitation year-round.
The subarctic classification of areas such as Hagfors and Torsby is more due to the cool summer nights that renders September below in mean temperatures.
Harva wrote the fourth volume of the book series The Mythology of All Races in 1927. It contains a classic general description of Subarctic shamanism.
Allakh-Yun has a monsoon-influenced, extreme subarctic climate (Koppen climate classification Dwd) with long, extremely cold and dry winters and short, very mild summers.
This allows it to invest more of its income (nutrients derived from prey) into long-term storage, compared to other subarctic Pinguicula which are income breeders and invest these nutrients into immediate plant size and flowering increases.Thorén, L. Magnus and Karlsson, P. Staffan (1998). Effects of supplementary feeding on growth and reproduction of three carnivorous plant species in a subarctic environment. Journal of Ecology; Jun98, Vol.
Chibougamau has a subarctic climate (Köppen climate classification Dfc), despite being located just south of 50 degrees latitude. Winters are long, cold, and snowy with a January high of and a low of . Summers are warm though short with a July high of and a low of . Overall precipitation is high for a subarctic climate with an average annual precipitation of and of snow per season.
This represents subarctic and subpolar oceanic climate realms, defined the same as in Köppen's scheme, where 1 to 3 months have an average temperature of or above. In this climate zone there is only a short period (normally 50 to 90 days) that is frost free. In the original scheme, this group was not further divided; later, the designations Eo and Ec were created, with Eo (maritime subarctic) signifying that the coldest month averages above , while Ec (continental subarctic or "boreal") means that at least one month has an average temperature of −10 °C or below. As in Group D, a third letter can be added to indicate seasonality of precipitation.
Averages from the no longer operational Dagali-Fagerlund and extremes. Back then, January averaged -8.9 and July averaged 10.8 making it still a subarctic (Dfc) climate.
Erdenet has a subarctic climate (Köppen climate classification: Dwc). Summers are typically warm and rainy with cool nights, while winters are long, very cold, and dry.
There are sparse forests of larch in river valleys and the mountain slopes are covered with mountain tundra. The climate of the Ilirney Range is subarctic.
Rhines, Peter, Sirpa Häkkinen, and Simon A. Josey. "Is oceanic heat transport significant in the climate system?." Arctic–subarctic ocean fluxes. Springer, Dordrecht, 2008. 87–109.
It is a pelagic species native to the North Pacific, although it migrates into Subarctic waters during the summer from its more southerly winter spawning grounds.
Sobolevo has a rare, dry-winter variant of subarctic climate (Köppen climate classification Dsc) with very long, bitterly cold winters and short, very mild and wet summers.
Arvidsjaur has a subarctic climate that is dominated by the long winters and briefly interrupted by moderately warm but very bright summers due to its northerly latitude.
Hordeum brevisubulatum is a widespread species of wild barley native to temperate and subarctic Eastern Europe and Asia. A halophyte, it prefers to grow in saline grasslands.
Poronaysk, owing to the cold Sea of Okhotsk surrounding the town, has a subarctic climate (Dfc) with short, mild and very foggy summers and very cold winters.
Lupin has a subarctic climate (Köppen Dfc) dominated by the cold and prolonged winter. Summers are short, but mild enough to bring it above a polar classification.
Shetland Islands Council Ferries (often named SIC Ferries) is a company operating inter-island ferry services in Shetland, a subarctic archipelago off the northeast coast of Scotland.
The climate at Yellowstone Lake is classified as subarctic (Dfc), according to Köppen-Geiger climate classification, while at the park headquarters the classification is humid continental (Dfb).
In spite of being located below the 50th parallel Matagami has a subarctic climate. The winter season is long and cold with a January daily mean of , but summer temperatures during the short season are quite warm for subarctic climates. On average around 133 days of the year do not have temperatures above freezing. The cold air is dominant with 224.4 days of the year averaging air frost.
Ayan has a subarctic climate (Köppen Dwc) with severe winters only marginally moderated by its maritime location and mild, wet summers. Its maritime location and favourable aspect for moist summer winds makes the coast around Ayan extremely wet for a subarctic climate and much wetter than interior Siberia, with an average annual rainfall more than four times that of Yakutsk and two-and-a-half times that of Chita.
Mackenzie has a subarctic climate that has influences from the Pacific Ocean resulting in less cold winters than expected for its northerly latitude compared to other Canadian locations. It has warm summer days, but the cool nights ensure that only three months go above in mean temperatures. Winters are very cold on occasion, although relatively short for a subarctic climate with a January mean of as the coldest month.
Kamenskoye has a subarctic climate (Köppen climate classification Dfc) with severely cold winters and mild summers. Precipitation is moderate and is heaviest in August and lightest in May.
Tok has a dry-winter continental subarctic climate (Köppen Dwc) with generally warm summers and severely cold winters. The weather station is at 1620 feet above sea level.
The Tagish language includes aspiration, glottalization, nasal sounds, resonance, and tones.Krauss, M. E., & Golla, V. K. (1978). Northern Athapaskan Languages. In Handbook of North American Indians: Subarctic (Vol.
Húsavík has a mild winter subarctic climate (Köppen: Dfc) or a subpolar oceanic climate (Cfc) depending on the isotherm used, or , similar to the rest of coastal Iceland.
The climate is continental (Koeppen Classification Dwc Subarctic climate: Snow climate with dry winter, cool summer and cold winter). 595 mm of precipitation per year (maximum in summer).
Cryocola is a genus of bacteria from the family of Microbacteriaceae with one known species (Cryocola antiquus). Cryocola antiquus has been isolated from subarctic tundra soil from Finland.
Soils of the subarctic are in which leaching of nutrients takes place even in the most heavily glaciated regions. The dominant soil orders are podsols and, further north, gelisols. Subarctic regions are often characterized by taiga forest vegetation, though where winters are relatively mild, as in northern Norway, broadleaf forest may occur—though in some cases soils remain too saturated almost throughout the year to sustain any tree growth and the dominant vegetation is a peaty herbland dominated by grasses and sedges. Typically, there are only a few species of large terrestrial mammals in the subarctic regions, the most important being elk, moose (Alces alces), bears, reindeer (Rangifer tarandus), and wolves (Canis lupus).
Salekhard has a subarctic climate (Köppen climate classification Dfc) with short, mild summers and severely cold winters. Precipitation is moderate, and is significantly greater in summer than in winter.
Oenopota is a boreal genus, with many species occurring in arctic and subarctic regions. They are less common in more southern waters where they occur in deeper, colder waters.
Amos has a humid continental climate (Köppen climate classification Dfb), just above a subarctic climate, with warm summers, very cold winters and heavy precipitation for most of the year.
6, pag. 143 The climate prevailing in the Syverma Plateau is severe, of the subarctic continental type with long, cold winters.Сыверма, Great Soviet Encyclopedia in 30 vols. / Ch. ed.
Based on the Köppen climate classification, Deltaform is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below .
Ust-Belaya has a continental subarctic climate (Köppen climate classification Dfc)McKnight and Hess, pp.232-5 with very long, bitterly cold winters and very short, somewhat cool summers.
Vinger has a subarctic climate (Dfc). September averages 9.7, falling just short of being the 4th month over 10 to fulfill the requirement for a humid continental climate (Dfb).
223–233 in Proc. Ecology of the Subarctic Regions, July–Aug. 1966, Helsinki, Finland, UNESCO. [Nienstaedt and Zasada 1990]Viereck, L.A.; Dyrness, C.T.; Van Cleve, K.; Foote, M.J. (1983).
Pickle Lake has a humid continental climate that closely borders on a subarctic climate (Köppen Dfb/Dfc) and actually used to have a subarctic climate, but not anymore due to global warming. Winters are cold and dry with a January high of and a low of . Most of the precipitation falls in the form of snow, averaging with reliable snow cover from November to April. There are 17.3 nights where the temperature will drop below .
The ecoregion is characterized by wet subarctic coniferous forest dominated by spruce and fir trees on the edge of tundra. The climate of Poronaysky is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ). In Poronaysky, there are over 100 rainstorms per year (average precipitation 600 mm/year), with frequent fog in the summer.
Baykit has a subarctic climate (Köppen climate classification Dfc) with bitterly cold winters and warm summers. Precipitation is moderate and is heavier in summer and fall than during other seasons.
Based on the Köppen climate classification, Mount Rhondda is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below .
Actaea, commonly called baneberry, bugbane and cohosh, is a genus of flowering plants of the family Ranunculaceae, native to subtropical, temperate and subarctic regions of Europe, Asia and North America.
Naryan-Mar has a subarctic climate (Köppen climate classification Dfc) with short, mild summers that may exceed and very cold winters. Precipitation is somewhat greater in summer than in winter.
Based on the Köppen climate classification, the range experiences a subarctic climate with cold, snowy winters, and mild summers. Temperatures in winter can drop below with wind chill factors below .
Protected by the Coast Mountains and with a high plateau, the climate is subarctic continental (Köppen: Dfc) with long cold winters and warm summers, but spring can be very dry.
C. canadensis can be found in many types of habitat, including forest, taiga, and tundra in subarctic regions. It is the most common and widespread Calamagrostis species on the continent.
The Holarctic species Rhodiola rosea is used in herbal medicine. A number of species are grown as ornamentals, but growing them is difficult outside their native subarctic and alpine climates.
Based on the Köppen climate classification, Maligne Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below .
Torpshammar has traditionally had a subarctic climate, although due to recent warming it is transitioning to a humid continental climate with four distinct seasons, cold winters and warm but short summers.
Lutsen Minnesota has a cold humid continental climate, just short of a Subarctic climate, as 4 months average above 10 degrees Celsius, one of which is only barely above that temperature.
East Glacier's climate is borderline Subarctic / Humid Continental, with warm summers, and winters generally beginning in November and lasting into March, bringing cold temperatures and over 176 inches of snowfall annually.
Trysil has a subarctic climate (Köppen Dfc) with cold winters and warm summers. Mean temperature in January is -11 °C and 14 °C for July. Precipitation is moderate at 720mm annually.
Subsequently, the journal's focus shifted to the north circumpolar region with emphasis on the Russian Arctic, publishing articles dealing with human as well as physical dimensions of Arctic and Subarctic environments.
Conifer has a subarctic climate (Koppen: Dfc) with a yearly temperature average of 38.6°F (3.7°C). Summertime is warm with cool nights, while winter is chilly with nights approaching zero.
Innbygda has a subarctic climate (Köppen Dfc) with cold winters and warm summers. Mean temperature in January is -10 °C and 14 °C for July. Precipitation is moderate at 795mm annually.
Fort McKay has a subarctic climate (Köppen climate classification Dfc). and falls into the NRC Plant Hardiness Zone 3a. Summers are mild and short, and winters can be long and cold.
Norway House has a subarctic climate (Dfc) bordering a warm summer continental climate (Dfb). As is typical in Manitoba, precipitation patterns are dominant in summers, with winters being cold and dry.
Based on the Köppen climate classification, Mount Kitchener is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below .
Despite its extreme latitude, more than north of the Arctic Circle, Sommarøya experiences an ocean-moderated subarctic climate (Cfc) with no month averaging below and a mean annual temperature of almost .
Like most of Labrador, Makkovik has a subarctic climate (Köppen Dfc) with short, mild summers and very cold winters; however, typically for its region but unusually for subarctic regions generally, precipitation is high with a minimum in the "spring" months from March to May. This high precipitation and cool summers is due to the powerful influence of the Icelandic Low and the Labrador Current on its western side, and gives very heavy snowfall of per year with an average maximum cover of during March and April. The greatest snow depth was on April 17, 1997. Unlike most places with a pronounced subarctic climate, Makkovik has a pronounced seasonal lag with August being much warmer than July and September averaging slightly warmer than June.
Kolpashevo has a subarctic climate (Köppen climate classification Dfc), with very cold winters and warm summers. Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Leushi has a subarctic climate (Köppen climate classification Dfc), with very cold winters and warm summers. Precipitation is moderate and is significantly higher in summer than at other times of the year.
Ivdel has a subarctic climate (Köppen climate classification Dfc), with very cold winters and warm summers. Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Drevsjø has a subarctic climate (Dfc) with only 3 months with a mean exceeding 10. There is a wetter period from June to September and a dry period from December to April.
Chalkyitsik has a continental subarctic climate (Köppen climate classification Dwc) with mild summers and cold winters. Precipitation is very low, but significantly higher in summer than at other times of the year.
Nizhneangarsk has a subarctic climate (Köppen climate classification Dfc), with severely cold winters and mild summers. Precipitation is moderate and is significantly higher in summer than at other times of the year.
Bureya has a subarctic climate (Köppen climate classification Dwc). characterized by cool summers, and very dry cold winters, moderated slightly in the case of Bureya by the relative proximity of the ocean.
Under the Köppen climate classification system, Prospect Creek has a subarctic climate. Prospect has recorded some of the coldest winters in U.S. history. There are currently no people living in this area.
Lukla has a subarctic climate (Köppen classification Dwc) with warm summers and very cold winters. There is high diurnal temperature variation, and temperatures can reach freezing even in the middle of summer.
Higher elevations feature a subpolar oceanic climate (Köppen: Cfc) with cool summers, cold winters, and constant rainfall that peaks during the winter months. The highest elevations feature a subarctic climate (Köppen: Dfc).
New Phytologist 174:864-878.Kjoller, R., M. Olsrud, and A. Michelsen. 2010. Co-existing ericaceous plant species in a subarctic mire community share fungal root endophytes. Fungal Ecology 3:205-214.
Bagdarin has a subarctic climate (Köppen climate classification Dwc) with severely cold winters and mild summers. Precipitation is quite low, but is much higher in summer than at other times of the year.
Swadling, K. M., J. A. E. Gibson, R. Pienitz, and W. F. Vincent. 2001. Biogeography of copepods in lakes and ponds of subarctic Quebec, Canada. Hydrobiologia 452/454:341-350.Torke, B. 2001.
Yessey has a subarctic climate (Köppen climate classification Dfc) with extremely cold winters and mild summers. Precipitation is quite low but is somewhat higher in summer than at other times of the year.
Based on the Köppen climate classification, it is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Paxson has a continental subarctic climate (Köppen Dfc), closely bordering on an alpine climate (Köppen ET) due to its high elevation and northerly latitude, with only one month above the 50 degree isotherm.
Chekunda has a monsoon-influenced humid continental climate (Köppen climate classification Dwb), closely bordering a subarctic climate; typified by extreme variation in seasonal temperatures, with warm, humid summers and severe to extreme winters.
Gamètì has a subarctic climate (Dfc) with the average high throughout the year averaging below the freezing point. Due to it being below the tree line it has relatively warm but short summers.
Novy Port has a severe subarctic climate (Köppen climate classification Dfc). The weather (even in the warmest month, July) is notoriously unpleasant. Winter lasts eight months, and precipitation is low throughout a year.
Based on the Köppen climate classification, it is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Castleguard is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Vitim has a subarctic climate (Köppen climate classification Dfc) with severely cold winters and warm summers. Precipitation is quite low but is somewhat higher in summer than at other times of the year.
Waskesiu experiences a borderline humid continental/subarctic climate (Köppen Dfb/Dfc). The highest temperature ever recorded in Waskesiu was on 5 June 1988. The coldest temperature ever recorded was on 21 January 1935.
Three Augochloropsis species are found in the temperate regions of North America (A. anonyma, A. metallica, and A. sumptuosa), but no species have managed to successfully exploit niches present in the subarctic zone.
The range has a harsh subarctic climate. The average temperature is . The coldest temperatures, down to , have been recorded in February. In summer the average July temperature in the valleys does not exceed .
The plateau has a harsh subarctic climate. The average temperature is . The coldest temperatures, down to , have been recorded in February. In summer the average July temperature in the valleys does not exceed .
Under the 1961-1990 normals, Gävle's fourth warmest month was just around the isotherm of to not be classified as subarctic, but temperatures did go up sufficiently to be clear humid continental since.
Imeni Poliny Osipenko has a humid continental climate (Köppen climate classification Dwb), closely bordering on a subarctic climate (Dwc) with dry, severely cold winters and warm, moist summers. As far as non-arid climates warmer than subarctic climates go, Imeni Poliny Osipenko is as cold as it gets, due to its low latitude and inland location enabling for the extended summers and four months to just go above . Winters are far colder than even many polar climates in maritime areas.
Seneca has a semi-arid influenced subarctic climate (Köppen climate classification Dsc) with warm daytime temperatures in summer and cool to cold nighttime temperatures all year. Average high temperatures throughout the year are relatively mild for a subarctic climate. It is right on the border of the regular semi-arid continental climate with the fourth warmest month of the year straddling . Seneca experiences the coolest weather in Grant County and has the distinction of the coldest official temperature recorded in Oregon: in 1933.
Before European colonisation, determining where a particular family or band could hunt, fish, and gather without encroaching on others to the point of over-harvesting was the main preoccupation of indigenous governance in the subarctic and other non-farming regions. Councils were convened to reconcile disputes and warfare was always a possibility. When European traders began exporting bulk amounts of fur to Europe in the eighteenth and nineteenth centuries, the trapping territories of the subarctic became much more commercially valuable and disputes intensified.
The Woodland Cree practised a Subarctic culture, and the Plains Cree a Plains culture and they spoke different but related dialects of the Cree language. Several peoples in Alberta fall under the term Dene, which is a name used by many related peoples in the Northwest Territories. In Alberta this includes the Beaver, Chipewyan, Slavey, and Sarcee. All Dene peoples share similar spiritual beliefs and social organization, but the Sarcee people are a Plains people, while the others are Subarctic.
During the mid-1960s, she also participated in several experiments designed to determine ocean current flows, using drift bottles in the subarctic Pacific Ocean and oceanographic data- gathering buoys equipped with radio transmitters released in the Pacific Ocean off the coast of Washington. In early 1966, she took part in the first winter oceanographic measurement of the Alaskan Stream – a current related closely to the formation of the salmon fishing ground – in the western subarctic region of the North Pacific.
The Ahtna are an Athabaskan languages speaking tribe of the Subarctic cultural area, which classifies them as both Athabaskan and Subarctic Indians. Depending on the community's location along the Copper River, dialectal differences may occur. The Lower Ahtna (Ahtna'ht'aene) are near the river's mouth which opens into the Gulf of Alaska, the Middle Ahtna (Dan'ehwt'aene) are upriver a distance, and the Upper Ahtna (Tate'ahwt'aene) live on the upper parts of the river. The Tanaina people of the west are their closest linguistic relatives.
Zhigalovo has a monsoonal subarctic climate (Köppen climate classification Dwc) with severely cold winters and warm summers. Precipitation is quite low, but is much higher in summer than at other times of the year.
Based on the Köppen climate classification, Mount Loudon is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Snow Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Lychnis Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Apex Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Alexandrovskoye has a subarctic climate (Köppen climate classification Dfc), with long, severely cold winters and short, warm summers. Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Suntar has a subarctic climate (Köppen climate classification Dfc), with short, warm summers and long, bitterly cold winters. Precipitation is low but is significantly higher in summer than at other times of the year.
Biser has a subarctic climate (Köppen climate classification Dfc), with very cold winters and mild summers. Precipitation is quite high, and is heavier in summer and autumn than at other times of the year.
Based on the Köppen climate classification, Mount Blakiston is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Mount Lambe is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Cirque Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Glacier Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Mount Daly is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Mount Bosworth is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
The climate present in Chignik is a typical subarctic climate (Köppen climate classification: Dfc), however it is mild when compared to other Alaskan towns with this climate type, for example Fairbanks or Fort Yukon.
Fairbanks’ climate is classified as subarctic (Köppen Dfc close to Dwc),University of Melbourne. “World map of Köppen-Geiger climate classification” . climate.gi.alaska.edu. Accessed October 4, 2009. with long cold winters and short warm summers.
Based on the Köppen climate classification, Terrapin Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Magog is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C.
Based on the Köppen climate classification, Mount Gloria is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Aye is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Eon Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Rico experiences an alpine subarctic climate (Köppen climate classification Dfc) with long, cold, very snowy winters and short, cool summers due to the high altitude and high precipitation year-round due to orographic lift.
Based on the Köppen climate classification, Mount Fay is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Mount Collie is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Boom Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, The Towers is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Myllyoja has a subarctic climate with cold, snowy winters and short, warm summers. Average annual temperature is . The average annual precipitation is falling on 98 days a year, mostly in late summer and fall.
Based on the Köppen climate classification, Mount Balfour is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Bourgeau is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, The President is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Gusty Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Whitehorn is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
According to the Köppen climate classification, Dillon has an alpine subarctic climate (Dfc). Summer days are usually warm, but with nights dropping close to freezing. Winter days are cold, with massive amounts of snowfall.
Based on the Köppen climate classification, Forum Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Mount Victoria is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Winters on the West Siberian Plain are harsh and long. The climate of most of the plains is either subarctic or continental. Two of the larger cities on the plain are Surgut and Nizhnevartovsk.
Based on the Köppen climate classification, Mount Columbia is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, it is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Pilot Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, The Fortress is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Slave Lake experiences a subarctic climate (Köppen climate classification Dfc) that borders on a humid continental climate (Köppen Dfb). Summers tend to be warm with cool nights while winters are long and severely cold.
Based on the Köppen climate classification, Mount Babel is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Nadina Mountain is located in a subarctic climate zone with cold winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Hungabee is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Diadem Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. .
Based on the Köppen climate classification, Mount Smythe is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Robertson is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Bident Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Chak Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C.
Ust-Barguzin has a subarctic climate (Köppen climate classification Dwc) with severely cold winters and mild summers. Precipitation is quite low and is significantly higher in summer than at other times of the year.
Based on the Köppen climate classification, Eiffel Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Elliott Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Aquila Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C.
Based on the Köppen climate classification, Angle Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Kista Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Mount Peskett is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Siffleur Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Allstones Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Pinnacle Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20°C with wind chill factors below −30°C.
Based on the Köppen climate classification, the mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Barguzin has a subarctic climate (Köppen climate classification Dwc), with severely cold winters and warm summers. Precipitation is quite low but is significantly higher in July and August than at other times of the year.
Chara has a subarctic climate (Köppen climate classification Dwc), with long, bitterly cold winters and warm, mild summers. Precipitation is quite low but is much higher in summer than at other times of the year.
Boguchany has a subarctic climate (Köppen climate classification Dfc) with severely cold winters and warm summers. Precipitation is quite low, but is somewhat higher from June to September than at other times of the year.
Based on the Köppen climate classification, Sentinel Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Dungeon Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Tilted Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, the mountain experiences a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C in the winter.
Based on the Köppen climate classification, Mount Gordon is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
The Tunguska Plateau is located in the permafrost zone and the soil never thaws at great depths.Олег Фейгин, Никола Тесла: Наследие великого изобретателя, p. 126 The climate prevailing in the Tunguska Plateau is subarctic continental.
Based on the Köppen climate classification, Mount Lawrence Grassi is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, Wenkchemna Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C in the winter.
Based on the Köppen climate classification, Nub Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Habel is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Hammarbya paludosa (or Malaxis paludosa) is a small orchid commonly known as bog orchid, bog adder's-mouth or bog adder's-mouth orchid. It grows in bogs in temperate and subarctic regions of the Northern Hemisphere.
Nizhneudinsk has a subarctic climate (Köppen climate classification Dwc), with long, severely cold winters and short, warm summers. Precipitation is quite low but is much higher in summer than at other times of the year.
Based on the Köppen climate classification, Mount Northover is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, the mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20° C with wind chill factors below −30° C.
Based on the Köppen climate classification, Trolltinder Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
The climate on the Kanin Peninsula has cold winters with moderate maritime influences and cool summers. The north has a tundra climate (ET) and the south a subarctic climate (Dfc) thanks to the warmer summers.
Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C in the winter.
Klyuchi has a typical subarctic climate (Köppen climate classification Dfc), albeit with slight early dry-summer precipitation patterns. Summers are generally mild and rainy with cool nights, while winters are long, cold, and very snowy.
Based on the Köppen climate classification, Wonder Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C.
Geilo features a Subarctic climate (Köppen Dfc) with cold winters and cool summers typical of higher altitudes (768m asl). The mean temperature in January is −8.2 °C and the mean for July is 11.2 °C.
Stevens Pass experiences a maritime-influenced alpine subarctic climate (Köppen Dsc), with short, mild, dry summers and extremely heavy winter snowfall. The following chart includes climate data from October 26, 1950 to April 30, 1994.
Like the rest of Maine the climate is warm-summer humid continental (Köppen: Dfb) bordering on a subarctic climate (Dfc), with cold and very snowy winters, and pleasant summers on a few occasions being hot.
Aklavik has a subarctic climate (Dfc), typical of Canada's Arctic, with mild summers and cold winters lasting most of the year with highs regularly below zero. Freezing can occur at any time of the year.
Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C in the winter.
Based on the Köppen climate classification, Brachiopod Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, the Opal Hills are located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, the mountain experiences a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C in the winter.
Based on the Köppen climate classification, Heather Ridge is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount William Booth is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
The English word "taiga" refers to a subarctic zone of evergreen coniferous forests, while the Japanese word means "(great) river". It is also possible for taiga to be the romaji form of the English word .
Based on the Köppen climate classification, Mount Tuzo is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C.
Based on the Köppen climate classification, The Mitre is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Under the Köppen climate classification, Lahti is right on the boundary between being a humid continental climate (Dfb) and a subarctic climate (Dfc). Summers are generally mild to warm, while winters are cold and snowy.
Based on the Köppen climate classification, Mount Dawson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Mackenzie is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Wheeler is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, this mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Topham is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Orion Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Scarab Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Zyryanka has a subarctic climate (Köppen climate classification Dfc and Dsc), with extremely cold winters and mild summers. Precipitation is quite low and is somewhat higher in summer than at other times of the year.
Based on the Köppen climate classification, Mount Woolley is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
The climate of Kurils is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ).
The climate of Tunguska is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ).
Based on the Köppen climate classification, Mount Whymper is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
Based on the Köppen climate classification, Mount Alexandra is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, this mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Ex Coelis Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Abraham Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Based on the Köppen climate classification, Mount Ernest Ross is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.
Narva has a warm-summer humid continental climate (Köppen climate classification Dfb) closely bordering on a subarctic climate (Dfc) with mild to warm, rainy summers with cool nights and very cold, cloudy and snowy winters.
Srednekolymsk has a dry and very cold subarctic climate (Köppen climate classification Dfc), bordering on an extreme subarctic climate (Köppen climate classification Dfd), featuring with mild, sometimes hot, even very hot, but short summers and extremely brutal winters with almost no snowfall. The winter lasts from October until May and temperatures rise rapidly enough for Siberian larch trees to be able to grow during the fleeting summer, before falling rapidly again in August and September. Temperatures often do not exceed between late September and early May.
The Hagfors area has a subarctic climate due to the area's cool nights. The official weather station is located in Gustavsfors, a rural locality to the north at a similar altitude. The climate type is very unusual for subarctic climate since summer days are warm in combination with winter average highs being just below freezing with lows only being around . Cold extremes are frequent for such a southerly area, with an all-time low of being unique for a Swedish area just north of 60 degrees latitude.
Nerchinsky Zavod has a subarctic climate (Köppen climate classification Dwc), with severely cold winters and warm summers. Precipitation is quite low but is somewhat higher from June to September than at other times of the year.
Waskesiu experiences a humid continental climate (Köppen Dfb) bordering on a subarctic climate (Dfc). The highest temperature ever recorded in Waskesiu was on 5 June 1988. The coldest temperature ever recorded was on 21 January 1935.
The lake is in the subarctic climate zone. The annual average temperature is . The warmest month is July, when the average temperature is and the coldest is January, with . The lake is surrounded by coniferous forest.
Androsace americana, synonym Douglasia arctica, known as the Mackenzie River dwarf primrose, is a species of flowering plant in the primrose family, Primulaceae. It is native to subarctic North America (Alaska, the Northwest Territories and Yukon).
Manasarovar lies above sea level, covers an area of and reaches a maximum depth of . Ngari has a cold desert climate (Köppen climate classification: BWk), with strong dry-winter subarctic climate tendencies (Köppen climate classification: Dwc).
Based on the Köppen climate classification, Mount St. Bride is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
Based on the Köppen climate classification, Mount Sir Douglas is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.
The Yukon Quest trail is in the subarctic climate range. In Fairbanks, the average February temperature is , but is not uncommon, and temperatures have dropped to . Alaska Climate Research Center. "Climatological data: Fairbanks International Airport" , climate.gi.alaska.edu.
Arctophila is a genus of Arctic and Subarctic plants in the grass family.Andersson, Nils Johan 1852. Plantas Scandinaviae Descriptionibus et Figuris analyticis Adumbratae. Fasciculus Secundus Gramineas Scandinaviae Complectens x, 48Kharkevich, S.S., Probatova, N.S. & Novikov, V.S. (1985).
Dashbalbar has a subarctic climate (Köppen climate classification Dwc) with warm summers and severely cold winters. Most precipitation falls in the summer as rain, with some snow in the spring and autumn. Winters are very dry.
Cochrane has a subarctic climate (Dfc) with very cold winters and warm summers. Diurnal temperature variation is moderately high throughout the year. Annual snowfall is heavy, averaging 117 inches (297 cm). Precipitation peaks during early fall.
Bodaybo has a subarctic climate (Köppen climate classification Dfc), with bitterly cold winters and warm summers. Precipitation is quite low, but falls mostly in summer, with the climate being arid at other times of the year.
Barkerville has a subarctic climate (Köppen climate classification Dfc), resulting in long, cold and snowy winters, accompanied by short and cool summers due to its high altitude and latitude. Its growing season averages only 66 days.
The climate of Turukhansk is classified as continental subarctic (Dfc) in the Köppen climate classification system and as continental sub- arctic (taiga) with mild summers and severely cold winters (ECld) in the Trewartha climate classification system.
Reykjahlíð features a tundra climate (Köppen climate classification: ET), bordering on a subarctic climate (Köppen climate classification: Dfc). Summers are typically cool with crisp nights while winters are very long and cold, but not severely cold.
As occasional individual black-legged kittiwakes have reddish legs, any reports of red-legged away from the subarctic Pacific must record all of the other differences, not just the leg colour, for acceptance by bird recording authorities.
Daniel's Harbour has a subarctic climate (Koppen: Dfc) with June being under the 50°F (10°C) isotherm. Summers are cool to mild while winters are chilly. Precipitation is heavy year round, though less heavy during Spring.
Its typical habitat is dense undergrowth or rocky areas in coniferous or birch forests, often near rivers, but it is also found in clear cut areas of forests, rough grassland, subarctic shrubby heathland and dry peat bogs.
Cantwell has a continental subarctic climate (Köppen Dfc), having mild summers with crisp nights and long, severely cold, and very snowy winters. On a midsummers day on July 17th, 2003, 6 inches of snow fell in Cantwell.
A high abundance of E. pandrose is a specific feature of the northern part of the Kanin Peninsula and Kolguev Island, pointing to the connection of the biota of these territories with the subarctic regions of Fennoscandia.
L'Étape experiences a borderline subarctic climate (Dfc) due to its elevation. Summer days are mild to warm with nights being cool. Winters are long and very cold. Springtime weather sometimes doesn't show itself until well into April.
Fort McPherson experiences a subarctic climate (Köppen climate classification Dsc). The highest temperature ever recorded in Fort McPherson was on 7 August 1919 and 20 July 2001. The coldest temperature ever recorded was on 14 January 1894.
Subarctic America: Greenland. Canada: British Columbia, New Brunswick, Newfoundland, Nova Scotia, Ontario, Prince Edward Island, Quebec. United States: Connecticut, Delaware, Maine, Massachusetts, Michigan, Minnesota, New Hampshire, New Jersey, New York, Oregon, Pennsylvania, Rhode Island, Vermont, Washington, Wisconsin.
Chalkyitsik is located at (66.651529, -143.727356). According to the United States Census Bureau, the CDP has a total area of , of which, of it is land and of it (3.76%) is water. Chalkystik has a bitter subarctic climate.
One dig uncovered hammerstones, iron pyrite nodules, scrapers and knives. The pyrite nodules showed signs of use as fire starters, struck against flint to create sparks. Plano Paleo-Indians likely hunted caribou, owing to the region's subarctic climate.
The Arctomiaceae are a family of lichenized fungi in the Ascomycota, class Lecanorales. The family was named by Theodor Magnus Fries in 1861. Species in this family are found in arctic and subarctic habitats, usually associated with bryophytes.
Subarctic rail transport only exists in Europe (lines to Narvik and Murmansk) and the Norilsk–Dudinka line in northern Siberia. An important consequence is that transportation tends to be restricted to "bush" planes, helicopters and, in summer, riverboats.
Pajala has a harsh subarctic climate that is somewhat moderated by the influence of the North Atlantic. Its inland position and lower elevation cause warmer summers, and winters are a bit milder than most areas on similar parallels.
Arctic and Subarctic tribes use sea grasses for basketry. At the dawn of the 20th century, Inupiaq men began weaving baskets from baleen, a substance derived from whale jaws, and incorporating walrus ivory and whale bone in basketry.
Belle Isle has a subarctic climate (Köppen climate classification Dfc) with short, cool summers and long, severely cold winters lasting most of the year. Precipitation peaks during the warmer months of June–September in the form of rain.
The climate of the Central Siberia Reserve is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ).
Skin boats dominated seafaring in places that were scarce on wood, including the arctic and subarctic. They were made by stretching skin or leather over frames of wood or bone. These include kayaks and umiaks, coracles and currachs.
The Small Moss Lake is not accessible to the public. The peat bog is very rich in spiders. Other species living here include alpine newt, Carpathian newt and moor frog. moorland clouded yellow and subarctic hawker are glacial relicts.
Zermatt has a subarctic climate (Köppen climate classification: Dfc). Summertime is very pleasant in Zermatt, with mild days and cool nights, while winter is cold and snowy, with highs around freezing and annual snowfall averaging 128 inches (325 cm).
Newfoundland is primarily characterized by having a subarctic (Köppen Dfc) or a humid continental climate (Köppen Dfb). Locations on the extreme southeast of the island receive sufficient maritime influence to qualify as having a subpolar oceanic climate (Köppen Cfc).
Khujirt has a subarctic climate (Köppen climate classification Dwc) with mild summers and severely cold winters. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
Anemonastrum richardsonii prefers subarctic climates and can be found in willow thickets, snow patches, along streams, near peat and mosses, and in moist areas with low drainage. It is capable of growing under a wide range of soil pH.
Influenced by its inland and northerly position, Jokkmokk's variety of a subarctic climate is very cold by Swedish standards. Summers are normally relatively mild in spite of the day-round light and the dark winters are long and cold.
P. antarctica is native to Antarctica. It is known from the Antarctic Peninsula, McMurdo Sound, the Ross Sea, South Georgia, Victoria Land and various subarctic islands. The type locality is Coulman Island near Cape Wadworth in the Ross Sea.
Based on the Köppen climate classification, Chapman Peak has in a subarctic climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Cornus suecica, the dwarf cornel or bunchberry, is a species of flowering plant in the dogwood family Cornaceae, native to cool temperate and subarctic regions of Europe and Asia, and also locally in extreme northeastern and northwestern North America.
Also nominated that year was Breaking the Ice: Stories from New Tibet, a collection set in and around a subarctic mining colony; Conway's contribution, "Dead End", features a bartending vulture who provides an introduction to the harsh, dystopic world.
Based on the Köppen climate classification, Cannon is located in a subarctic climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Vaccinium ovalifolium (commonly known as Alaska blueberry, early blueberry, oval-leaf bilberry, oval-leaf blueberry, and oval-leaf huckleberry) is a plant in the heath family having three varieties, all of which grow in northerly regions, including the subarctic.
Ukhta has a continental subarctic climate (Dfc) with long, cold winters and short, warm summers. Compared with areas at a similar latitude in Siberia, winters are less extreme, but still much longer than summer and bitterly cold by European standards.
The Pekulney Range has a barren look. The mountain slopes are covered with very little vegetation, mainly grasses, shrubs and "dwarf cedar", up to to . At higher elevations there is only rocky mountain tundra. The climate of the area is subarctic.
Cape Newenham has the typical subarctic climate of most of Alaska, though owing to the maritime influence of the Bering Sea it borders on a polar climate despite receiving an amount of precipitation one would expect more of an oceanic location.
Anne Applebaum — Inside the Gulag The infamous complexes were those at Kolyma, Norilsk, and Vorkuta, all in arctic or subarctic regions. However, prisoner mortality in Norilsk in most periods was actually lower than across the camp system as a whole.
Port Heiden is located at (56.948949, -158.655745). According to the United States Census Bureau, the city has a total area of , of which, of it is land and of it (1.28%) is water. Port Heiden has a subarctic climate (Köppen Dfc).
Faro has a subarctic climate (Köppen Dfc) with mild summers and severely cold winters. Extreme seasonal swings are common, although less severe than farther east in Canada due to the warm spells in summers and occasional mild spells in winter.
Burgess Junction experiences a subarctic climate (Köppen Dfc) with long, bitter and snowy winters and cool summers. It is the snowiest inhabited place in Wyoming. March holds the highest annual snow depth of any month, averaging 34 inches (86.4 cm).
Based on the Köppen climate classification, Heavy Runner Mountain is located in a subarctic climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Based on the Köppen climate classification, Manx Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Manx Peak drains into the Athabasca River.
Based on the Köppen climate classification,Mount Nestor is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains into the Spray Lakes Reservoir.
Fort Severn has a subarctic climate (Dfc) and is one of the coldest communities in Ontario. Summers typically have cool to mild weather with short heatwaves, while winters are severely cold and long, lasting from October to sometimes through May.
Based on the Köppen climate classification, Mount Shark is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains west into Spray Lakes Reservoir.
Tara has a humid continental climate (Köppen climate classification Dfb) bordering on a subarctic climate (Köppen Dfc), with very cold winters and mild summers. Precipitation is quite low, but is significantly higher in summer than at other times of the year.
The family Orobanchaceae has a cosmopolitan distribution, found mainly in temperate Eurasia, North America, South America, parts of Australia, New Zealand, and tropical Africa. The only exception to its distribution is Antarctica, though some genera may be found in subarctic regions.
Based on the Köppen climate classification, it is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures in winter can drop below with wind chill factors below . Weather conditions during summer months are optimum for climbing.
Based on the Köppen climate classification, Mount Girouard is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains into the Bow River.
Based on the Köppen climate classification, Stanton Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Fairplay has a subarctic or subalpine climate (Koppen: Dfc) given its elevation, with short but warm summers, and long, snowy, moderately cold winters. Temperature ranges between day and night are large, due to the high elevation and dryness of the air.
Harbour porpoises prefer temperate and subarctic waters. They inhabit fjords, bays, estuaries and harbours, hence their name. They feed mostly on small pelagic schooling fish, particularly herring, capelin, and sprat. They will, however, eat squid and crustaceans in certain places.
Malung has a relatively moderate subarctic climate not far below continental. In comparison with areas further east in the county like Falun, temperatures are generally chilly. Cold extremes in particular are very cold by standards this far south in the country.
Based on the Köppen climate classification, Longfellow Peak is located in a subarctic climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Climate type is dominated by the winter season, a long, cold period with short, clear days, relatively little precipitation mostly in the form of snow, and low humidity. The Köppen climate classification subtype for this climate is "Dfc"(Continental Subarctic Climate).
Lake Louise experiences a subarctic climate (Köppen climate classification Dfc). Annual snowfall averages 3.3m and winter temperatures below −50 °C have been recorded. Summers consist of frosty mornings and crisp, cool days. Snow can occur in any month of the year.
Athabasca experiences a humid continental climate (Köppen climate classification Dfb) that borders on a subarctic climate (Köppen Dfc). The highest temperature ever recorded in Athabasca was on July 18, 1941. The coldest temperature ever recorded was on January 11, 1911.
Northern Labrador's climate is classified as polar, while Southern Labrador's climate is classified as subarctic. Labrador can be divided into four geographical regions: the North Coast, Central Labrador, Western Labrador, and the South Coast. Each of those regions is described below.
The region's climate is subarctic. Winters are long and last, on average, from October 22 to May 4. Summers are short and mild, with temperatures averaging in July, while dropping to in January. Annual precipitation average , a third in snow.
Khatgal experiences a subarctic climate (Köppen Dwc) with very long, very dry, frigid winters and short, cool, relatively wet summers. Sunshine is abundant year-round and is especially high during the winter for a location above the 50th parallel north.
Data for nearby Bråtå weather station. Bismo has a dry summer subarctic climate (Dsc). Spring is the driest time of year and fall and winter are the wettest. The coldest month, January, averages -8.8 while the warmest month, July, averages 11.7.
Belozersk falls just within the subarctic climate range, with the fourth-warmest month being just below the isotherm of to nearby humid continental areas. Winters are cold but not severe by Russian standards for areas north of the 60th parallel.
Based on the Köppen climate classification, Olsen Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10° F with wind chill factors below −30° F.
Island Park has a humid continental climate (Dsb), bordering on a subarctic climate (Dsc). Summer days are usually warm, with nights dropping to temperatures around 40, while winters are very cold, with massive yearly snowfall averaging 215 inches (546 cm).
Fogo Island has a marine-based cold humid continental climate (Dfb) bordering on subarctic (Dfc) with cooler summers than inland areas of Newfoundland as well as milder winters than areas on the same parallels in interior Canada. However, due to the very cool characteristics of summer months, Fogo Island in many ways resembles the subarctic range. The fourth warmest month of June just straddles in mean temperature. As typical of Newfoundland and its surroundings precipitation is high and consistent year-round, which results in more three and a half metres of snowfall on average in winter.
Subarctic vegetation in Canada (Larix laricina) Subarctic temperatures are above for at least one and at most three months of the year. Precipitation tends to be low due to the low moisture content of the cold air. Precipitation is typically greater in warmer months, with a summer maximum ranging from moderate in North America to extreme in the Russian Far East. Except in the wettest areas glaciers are not large because of the lack of winter precipitation; in the wettest areas, however, glaciers tend to be very abundant and Pleistocene glaciation covered even the lowest elevations.
Sept-Îles has a subarctic climate (Köppen climate classification Dfc) bordering on a humid continental climate (Dfb) despite being located at around only 50 degrees latitude. The two main seasons are summer and winter, as spring and autumn are very short transition seasons lasting only a few weeks. Winters are long, cold, and snowy, lasting from late October to late April, but milder than more inland locations, with a January high of and a January low of . Overall precipitation is unusually high for a subarctic climate, and snow totals correspondingly heavy, averaging per season with an average maximum depth of .
Cree is believed to have begun as a dialect of the Proto-Algonquian language spoken between 2,500 and 3,000 years ago in the original Algonquian homeland, an undetermined area thought to be near the Great Lakes. The speakers of the proto-Cree language are thought to have moved north, and diverged rather quickly into two different groups on each side of James Bay. The eastern group then began to diverge into separate dialects, whereas the western grouping probably broke into distinct dialects much later.Rhodes and Todd, "Subarctic Algonquian Languages" in Handbook of North American Indians: Subarctic, p.
They are small, herbaceous plants, mostly of arctic and subarctic regions, but a few extend further south, and one genus is endemic to northern South America and Florida. Tofieldia pusilla is sometimes grown as an ornamental.Anthony Huxley, Mark Griffiths, and Margot Levy (1992).
Based on the Köppen climate classification, Mount Wright has a subarctic climate (Dfc) with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into Glacier Bay Basin.
Tomsk has a humid continental climate (Köppen climate classification Dfb) barely escaping a subarctic classification. The annual average temperature is . Winters are severe and lengthy, and the lowest recorded temperature was in January 1931. However, the average temperature in January is between and .
Based on the Köppen climate classification, Oppy Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Weather conditions during summer months are optimum for climbing.
Tulun has a subarctic climate (Köppen Dfc) with mild to warm, humid summers and severely cold, drier winters. The monthly 24-hour average temperature ranges from in January to . Sunshine is generous and the area receives 2,237 hours of bright sunshine annually.
The genus Brama is predominately pelagic and can be found globally in the high seas, with the exception of arctic and subarctic waters. This is true with the exception of two species, Brama orcini and Brama dussumieri, which occupy shallower waters surrounding landmasses.
It is at mile 412 of the Alaska Railroad. The river is ice-free from early May to late October. Nenana has a continental subarctic climate (Köppen Dfc) with long, severely cold and dry winters and short, warm summers with cool nights.
Based on the Köppen climate classification, Cheops Mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into the Illecillewaet River.
Based on the Köppen climate classification, Little Chief Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
He reached York Factory on Hudson Bay via the Hayes River in June 1742. He was traveling with a large band of Indians and several canoes full of furs for trade. The successful mission opened the British fur trade with the subarctic.
Based on the Köppen climate classification, Mount Edith is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Weather conditions during summer months are optimum for climbing.
Based on the Köppen climate classification, it is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Weather conditions during summer months are optimum for climbing.
Based on the Köppen climate classification, Mount Fifi is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Weather conditions during summer months are optimum for climbing.
Syktyvkar experiences a subarctic climate (Köppen climate classification Dfc) with long, cold winters and short, warm summers. Compared with areas at a similar latitude in Siberia, winters are less extreme, but still much longer than summer and bitterly cold by European standards.
Some hills and peaks in the province, especially around the Sarıkamış region, are subarctic (Köppen climate classification Dfc) due to the higher elevation of the region. Both the summers and winters are colder in this area, with winter temperatures reaching more regularly.
More than two-thirds of the annual rainfall occurs during the three summer months. The Mohe-Huma-Hailar triangle between northern Heilongjiang and Northeastern Inner Mongolia, which almost equivalent to China's subarctic climate zone, suffers the most severe cold winter in China.
1915-1920 as an early winter camp from October to January. The known distribution of earth-covered conical lodges in the eastern Subarctic extends from the east coast of James Bay at the Eastman River post, the lower Rupert River, and Fort George.
Near the summer solstice for instance, subarctic regions experience an all night period of either civil, nautical, or astronomical twilight, since the sun never dips more than 18 degrees below the horizon. Noctilucent clouds are best observed within this range of latitude.
Roberval has a cold and highly seasonal humid continental climate (Köppen Dfb), with mild summers, cold winters and high annual snowfall. Due to seasonal lag and influence from the nearby lake, September is well above the subarctic threshold as the fourth warmest month.
Timmins, the nearest urban centre, is located approximately south. Moosonee is south of Attawapiskat. It is located 52°55′ north and 82°26′ west. The vegetation is typically subarctic with a mostly coniferous forest (stunted black spruce and tamarack) in the muskeg.
Upsalquitch Lake has a subarctic climate (Dfc). Summers are typically rainy and mild, with a handful of warm days. Nighttime temperatures remain cool. Winters are some of the longest, coldest and snowiest in New Brunswick, with annual snowfall averaging 130 inches (330 cm).
Dodia is a genus of woolly bear moths in the family Erebidae. The genus was erected by Harrison Gray Dyar Jr. in 1901. The moths are found in subarctic tundra and taiga ecosystems. They belong to the subtribe Callimorphina of tribe Arctiini.
Vanavara has a subarctic climate (Köppen climate classification Dfc). Winters are severely cold with average temperatures from in January, while summers are warm with average temperatures from . Precipitation is moderate and is somewhat higher in summer than at other times of the year.
The only maintained trail to the summit is the Humphreys Trail, a strenuous hike that starts at Arizona Snowbowl.Humphreys Peak on Summitpost.org Towards the top of the trail Humphreys Peak contains the only area of subarctic tundra south of the Rocky Mountains.
The slopes are covered by sparse larch taiga up to between and , above which grow Siberian pine thickets. The higher elevations have only mountain tundra. The zone of the Angachak Range has a harsh continental subarctic climate. January temperatures vary from to .
An early project using EMC made from fly ash was the construction of a road bridge in Karungi, Sweden, in 1999, with Swedish construction firm Skanska. The Karungi road bridge has withstood Karungi's harsh subarctic climate and divergent annual and diurnal temperature ranges.
Fort Chipewyan has a subarctic climate (Köppen Dfc) with long, very cold, dry winters and short, warm, wetter summers. The highest temperature ever recorded in Fort Chipewyan was on 27 June 2002. The coldest temperature ever recorded was on 1 February 1917.
Based on the Köppen climate classification, Cromwell is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from the mountain drains into the Athabasca River.
It is a bee of alpine and subarctic climates. It lives in open, grassy habitat such as mountain meadows. It nests underground, or sometimes on the surface. Its food plants include sandworts, rabbitbrush, fireweeds, lupines, coyote mints, butterburs, mountain heathers, and groundsels.
The bowhead whale is the only baleen whale to spend its entire life in the Arctic and subarctic waters.Moore, S. E., and R. R. Reeves (1993). "Distribution and Movement". In Burns, J. J.; Montague, J. J.; and Cowles, C. J. The Bowhead Whale.
Thompson Pass has an alpine tundra climate (ET) with one of the highest snow totals in the world. In spite of its high latitude, it retains a mediterranean precipitation pattern, with dry summers, although those are too cool to qualify for dry-summer subarctic.
Based on the Köppen climate classification, Midgard Peak has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.
Based on the Köppen climate classification, Gimli Peak has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.
The defined climate is a subarctic continental (Köppen: Dfc). Because of its northern location, winters are long, snowy, cold, and dark. During midwinter, the city receives daylight for only around five hours. Summers are mild, with the average daily maximum temperature being in July.
Bulgan experiences a subarctic climate (Köppen climate classification Dwc) with mild summers and severely cold winters. Precipitation is very low, but significantly higher in summer than at other times of the year. Winters are very dry, although some snowfall occurs around April and October.
Ust-Tsilma has a subarctic climate (Köppen climate classification Dfc). Winters are very cold with average temperatures from in January, while summers are mild with average temperatures from . Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Elkwater experiences a subarctic climate (Köppen climate classification Dfc) that falls just short of the boundary with the humid continental climate zone (Köppen Dfb). Winters are long and cold, while summers are short and warm. Precipitation is moderate, with an annual average of 529mm.
Lourdes-de-Blanc-Sablon has a subarctic climate (Köppen Dfc) that is influenced by the surrounding sea, moderating summer temperatures, and also ensuring winters are less severe than inland, although this region of Quebec is severely cold annually by global standards for the latitude.
This difference in precipitation between the lower and higher elevations of forested areas spans two Köppen climate classifications. The majority of the Fremont is Csb: warm summer Mediterranean, whereas elevations of 7,000 feet and higher are designated as Dsc: dry summer subarctic, (Climate Data.org 2016).
Due to its high elevation, Bondurant experiences a subarctic climate (Köppen Dfc). Winters are long and cold, sometimes severely cold, and snowy, with annual snowfall averaging . Summers are short and warm, sometimes hot. Precipitation is heaviest in winter, but fairly even throughout the year.
Batagay-Alyta has an extremely cold subarctic climate (Köppen climate classification Dfd) with long, extremely cold winters and short, mild (sometimes warm) summers. The seasonal temperature variation is among the greatest in the world. Precipitation is very low, but somewhat higher in the summer.
Magadan is located in the Cherskii-Kolyma mountain tundra ecoregion. This ecoregion covers the mountainous areas of northeast Siberia. It is an ecoregion of extreme cold and extreme aridity. The climate of Magadan is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)).
Waterton Lakes National Park Cameron Falls weather station has a humid continental climate (Koppen: Dfb), bordering relatively closely on a subarctic climate (Dfc). Summertime is mild with cool nights, while winter is chilly with highs around freezing. Snowfall is heavy, averaging 481.5 cm (189.6 inches).
The climate of Alakanuk is subarctic, averaging of snowfall and of total precipitation per year. Temperatures range from between . Heavy winds are frequent during the fall and winter. The Yukon River is used as an ice road during freeze-up, from November through May.
The History of Shetland concerns the subarctic archipelago of Shetland in Scotland. The early history of the islands is dominated by the influence of the Vikings. From the 14th century it was incorporated into the Kingdom of Scotland, and later into the United Kingdom.
Though much of the Stikine Region is unprotected, the area's remoteness and unusual subarctic landscapes, and location along one of only two overland routes to the Yukon and Alaska, are attracting a growing amount of tourist traffic and generating employment in outfitting, guiding and hunting.
The area which is forested constitutes a much greater area than cultivated lands. Balagansk has a subarctic climate (Köppen climate classification Dfc). Winters are very cold and long while summers are warm and wet. Average monthly temperatures range from in July to in January.
Based on the Köppen climate classification, Indian Ridge is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Indian Ridge drains into tributaries of the Miette River and Athabasca River.
Based on the Köppen climate classification, Naiset Point is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Naiset Point drains into Lake Magog.
Kalevala has a subarctic climate. Its climate is somewhat tempered by its relative proximity to mild marine areas, ensuring winters that are more habitable than areas further east. However, in spite of this, the winter season is dominant and summers are short and cool.
According to the Köppen climate classification, Nowy Targ straddles the border of the Warm Summer Continental (Dfb) and Subarctic (Dfc) climates, with most of the city falling in the Dfb group. The Dfc climate is only found above 800 metres of elevation within Nowy Targ.
Nordegg has a subarctic climate (Dfc) which can be considered a subalpine climate due to its altitude with locations on the same latitude having warmer climates. Summers are mild, with a few warm days sprinkled in here and there, while winters are cold and snowy.
Peawanuck has a subarctic climate (Dfc) due to its location in far Northern Ontario, which brings long cold winters and short but mild summers. Peawanuck is one of the coldest communities in Ontario, having far different weather than the more populous parts of Ontario.
Based on the Köppen climate classification, Evelyn Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Evelyn Peak drains into the Athabasca River.
Based on the Köppen climate classification, Mount Kerkeslin is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Kerkeslin drains into the Athabasca River.
Based on the Köppen climate classification, O'Malley Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into Campbell Creek.
For nearby Fokstugu at 973 masl. The climate here is borderline subarctic (Dfc). Although the wet season is in summer, the driest time of year is in late spring. An extra 3 mm in October would give it 3 times the precipitation of April.
Kilpisjärvi has a subarctic climate (Köppen climate classification: Dfc). Summertime is generally cool and rainy with crisp nights, but can be mild. Winter is very cold and snowy and typically begins during late September or early October, and can last well into May some years.
The daily mean temperatures of the Grand Forks winters are associated with subarctic climates with frequent subzero temperatures. Due to the extended warm period of daily means above from May to September, the city's climate is still classified within the humid continental temperature range.
Biogeografiya Beringiyskogo Sektora Subarktiki (Biogeography of the Beringian sector of the Subarctic). Vladivostok: Izd-co DVNTs, 1986, pp. 122-145. along with Arctic char, although the community of char is infested with Acanthocephala. Similar fish exist in the Ust-Chaun region,Andreev, A.V. p.
Khonuu has an extreme subarctic climate (Köppen climate classification Dfd). Winters are extremely cold with average temperatures from in January, while summers are cool with average temperatures from . Precipitation is quite low and is somewhat higher in summer than at other times of the year.
Waryfishes are deep-sea aulopiform fishes in the small family Notosudidae. They are thought to have a circumglobal distribution in subarctic to subantarctic waters. The family name Notosudidae derives from the Greek noton (back) and Latin sudis (a fish, esox, the name of salmon).
Scofield has an alpine subarctic climate (Köppen Dfc) with enormous yearly snowfall in its long, cold winters due to its location in the Wasatch Range. Summertime on the other hand is pleasant, with warm days and crisp, cool nights hovering not too far above freezing.
Several biogeographic factors contribute to the richness and diversity of Saskatchewan flora. From north to south there are a variety of vegetative zones. To the far north are the Subarctic Woodland and Northern Boreal Forest. The Southern Boreal Forest is south of the treeline.
Waterton Park has a humid continental climate (Köppen Dfb), just above the subarctic climate (Dfc). Summers are mild with cool nights, while winters are chilly with highs around freezing. Precipitation is relatively consistent year round, but peaks during the months of May and June.
Based on the Köppen climate classification, Brussels Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from Brussels Peak drains into the Athabasca River.
Based on the Köppen climate classification, Buller is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the mountain drains west into Spray Lakes Reservoir.
Based on the Köppen climate classification, Mount Dungarvan is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of Waterton River.
Based on the Köppen climate classification, Mount Rogers has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Beaver River.
Based on the Köppen climate classification, The Steeples has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Kootenay River.
The Trans-Siberian Railway, which skirts the edge of the region, provided a major boost to Russian settlement in the subarctic, as did the intensive industrialization under Joseph Stalin that relied on the enormous mineral resources of the Central Siberian Plateau. Today, many towns in subarctic Russia are declining precipitously as mines close. In Canada, after the early minerals ran out, development stalled until hydroelectric development occurred in the 1950s and 1960s. Hydro-Quebec in particular has carried out many engineering works in regions of near-continuous permafrost, but these have never supported a significant population and have mainly served densely populated southern Quebec.
Plains bands could often congregate into large, pan-tribal hunting or war parties, especially once horses were available, due to the abundant supply of bison for food and the open, easily traversed landscape. As well, bands could migrate over vast distances, following the bison or for military purposes. Subarctic peoples also migrated, but in much smaller groups since the productivity of the boreal forests is so low that it cannot support any large groups in one place for long. Migrations in the subarctic would include following traplines, snowshoeing onto frozen lakes for ice fishing, searching moose and other game, and returning to favourite berry patches.
Kanchalan has a continental subarctic climate (Dfc).McKnight and Hess, pp. 232–235 It experiences extremely cold winters. Temperatures generally do not rise above freezing between the beginning of October and the following May and are generally below between the beginning of December and the following March.
Bicycle routes have been specified outside the nature reserve in nearby forests. The subalpine climate may change to subarctic condition and hence when taking adventure walks in the night through the park it could be hazardous unless one is properly equipped for taking such a risk.
Based on the Köppen climate classification, Mount Nelson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Nelson drains into tributaries of the Columbia River.
Based on the Köppen climate classification, Mount Fryatt is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Fryatt drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Highbush Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a small unnamed glacier on its east slope.
Based on the Köppen climate classification, Mount Selkirk is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Vermilion River.
Based on the Köppen climate classification, Mount Afton is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains north into the Illecillewaet River.
Based on the Köppen climate classification, Mount Green is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains north into the Illecillewaet River.
Although snowfall usually occurs from November to April, in the nearby village of Spinkabo measurable snowfall was observed on 30 September 1995 (12 cm) and 14 June 1982 (7 cm). Since only three months have an mean daily temperature exceeding 10°C, the climate qualifies as subarctic.
Bor has a subarctic climate (Köppen climate classification Dfc). Winters are severely cold with average temperatures from in January, while summers are warm with average temperatures from in July. Precipitation is moderate and is somewhat higher in summer and autumn than at other times of the year.
The rural okrug has an extreme subarctic climate (Köppen climate classification Dfd). Winters are extremely cold with average temperatures from in January, while summers are mild with average temperatures from . Precipitation is moderate, and is significantly higher in summer than at other times of the year.
Thus the paludification process includes a shift from forests, grassland or long exposed bare land to peatland.Kuhry, P., Turunen, J., 2006. The postglacial development of boreal and subarctic peatlands. In: Wieder, R.K., Vitt, D.H. (Eds.), Boreal Peatland Ecosystems (Ecological Studies), Springer Berlin Heidelberg, Germany, 25-46.
Oulu has a subarctic continental climate (Köppen: Dfc). It is the largest Finnish city entirely in this climatic zone as well as one of the largest such in the world. The typical features are cold and snowy winters with short and warm summers. Average annual temperature is .
Daniel is located at (42.865172, −110.070921). According to the United States Census Bureau, the CDP has a total area of 5.1 square miles (13.2 km2), all of it land. Daniel experiences a dry subarctic climate (Köppen Dfc) with long, cold, dry winters and short, warm summers.
The first works of Alain Testart treat the social organization of the Australian Aborigines and of the hunter- gatherers, peoples who did not engage in any form of agriculture or animal herding at the time of colonization (Australian Aboriginals, San, arctic and subarctic American Indians, Pygmies, etc.).
Rivière-au-Tonnerre has a subarctic climate (Dfc) with mild summers, rainy autumns and long, cold and snowy winters with annual snowfall averaging 99 inches (251 cm). Winter typically starts in late October or early November and lasts through most of, if not all of April.
Natashquan experiences a borderline subarctic climate (Köppen Dfc) that is just short of being classed as a humid continental climate (Köppen Dfb). Summers are mild, moderated by the Gulf of St Lawrence and winters are cold and snowy, with annual snowfall averaging 140 inches (356 cm).
Strip along the coast up to 30 km developed marine terraces. The climate is temperate continental, subarctic in the north. In the north is dominated by tundra (Bolshezemelsky, Malozemelskaya, and Timan tundra), in the south - the coniferous forests, watersheds, and swamps. There are deposits of coal, oil.
Sretensk has a very continental subarctic climate (Köppen climate classification Dwc) bordering closely on a humid continental climate (Köppen climate classification Dwb), with severely cold winters and warm summers. Precipitation is quite low but is much higher in summer than at other times of the year.
Unalakleet is located at (63.878907, -160.789680). Unalakleet is located on the Norton Sound of the Bering Sea at the mouth of the Unalakleet River, southeast of Nome and northwest of Anchorage. Unalakleet has a subarctic climate (Koppen: Dfc) with considerable maritime influences. Winters are cold and dry.
Chulman has a subarctic climate (Köppen climate classification Dfc/Dwc). Winters are bitterly cold with average temperatures from in January, while summers are mild with average temperatures from in July. Precipitation is moderate and is much higher in summer than at other times of the year.
Pelly Crossing has a severely continental subarctic climate (Dfc) with short but warm summers, but with the vast majority of the year being dominated by the bitterly cold winters. During cold snaps temperatures approaching has been recorded. The weather is rather dry and summer nights remain cool.
Kirensk has a subarctic climate (Köppen climate classification Dfc). Winters are severely cold with average temperatures from to in January, while summers are warm with average temperatures from to . Precipitation is quite low and is significantly higher in summer than at other times of the year.
Based on the Köppen climate classification, Mount Carnarvon is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Carnarvon drains into tributaries of the Kicking Horse River.
Based on the Köppen climate classification, Eagle Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Eagle Mountain drains into tributaries of the Bow River.
Babine- Witsuwitʼen is classified as Northern Athabaskan, in the same linguistic subgrouping as Dakelh and Chilcotin (though the latter is far more distinctly separate from Babine-Witsuwitʼen).Krauss, Michael E. and Victor Golla (1981) Northern Athapaskan Languages. Handbook of North American Indians, Vol. 6: Subarctic, ed.
Ust-Maya has an extreme subarctic climate (Köppen climate classification Dfd). Winters are extremely cold with average temperatures from in January, while summers are warm with average temperatures from . Precipitation is quite low and is somewhat higher in summer than at other times of the year.
Accessed March 14, 2009. The trail for the Yukon Quest 1,000-mile sled dog race passes over the mountain every February. The mountain is in a subarctic climate region, and is covered by an average snowpack of during March and April.Alaska Snow, Water, and Climate Services.
Based on the Köppen climate classification, Skogan Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Bow River.
Based on the Köppen climate classification, Mount Richards is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Richards drains into Waterton Lake, thence Waterton River.
The species was first described by Pieter Cramer in 1776. The species is widespread in continental North America, with local populations found throughout subarctic Canada and the United States. The caterpillar can eat 86,000 times its weight at emergence in a little less than two months.
Khatyryk-Khomo has an extreme subarctic climate (Köppen climate classification Dwd). Winters are extremely cold with average temperature of in January, while summers are mild to warm, with average temperature of in July. Precipitation is quite low in winters, being mostly concentrated in summer and early autumn.
Based on the Köppen climate classification, Mount Astley is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Astley drains into tributaries of the Bow River.
Based on the Köppen climate classification, The Ramp is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into Ship Creek and Campbell Creek.
Based on the Köppen climate classification, Parker Ridge is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Parker Ridge drains into tributaries of the North Saskatchewan River.
Based on the Köppen climate classification, Cockscomb Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Bow River.
Based on the Köppen climate classification, Mount Inglismaldie is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Inglismaldie drains into Lake Minnewanka and the Bow River.
Based on the Köppen climate classification, Mount Williwaw is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into Ship Creek and Campbell Creek.
Based on the Köppen climate classification, Sunburst Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20° C with wind chill factors below −30° C. Precipitation runoff from the peak drains into headwaters of the Mitchell River.
Based on the Köppen climate classification, The Marshall is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20° C with wind chill factors below −30° C. Precipitation runoff from The Marshall drains into tributaries of the Mitchell River.
In the Volga-Kama area and more northerly the culture extends to the Pechora River and Subarctic Ural. In the Volga and Lower Kama areas the traces of the Ananyino Culture fade in the 6th century BCE, in other areas in the 3rd to 2nd centuries BCE.
Red River has a humid continental climate (Koppen: Dfb), bordering on a subarctic climate (Dfc) with four seasons. Summertime is very warm with refreshingly cool nights, and winter is cold, but not extremely cold, with massive amounts of snowfall, averaging 147 inches (372 cm) a year.
Tayshet has a subarctic climate (Köppen Dfc) bordering on a humid continental climate with warm, humid summers and severely cold, drier winters. The monthly 24-hour average temperature ranges from in January to . Sunshine is generous and the area receives 2,150 hours of bright sunshine annually.
Leduc experiences a humid continental climate (Köppen Dfb) closely bordering on a subarctic climate (Dfc). Summers are typically warm and rainy with cool nights. Winters are typically long, very cold, and very dry with moderate snowfall. Precipitation usually peaks during July, which is also the sunniest month.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Monkhead is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Monkhead drains into the Maligne River, which is a tributary of the Athabasca River.
During the deglaciation following the Last Glacial Maximum, northwestern Eurasia experienced widespread flooding from the Atlantic Ocean to the Yenisei River, including the subarctic and Himalayas: over . Flooding occurred in four landforms: marine lowlands, river valleys, watersheds and slopes, and peaked 17,000 to 15,000 years ago.
Based on the Köppen climate classification, Mount Hector is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Hector drains into tributaries of the Bow River.
Fort Good Hope experiences a subarctic climate (Dfc), with long, cold winters and short, warm summers. The highest temperature ever recorded was on 20 June 1911, 11 July 1920 and 5 July 1998. The coldest temperature ever recorded was on 31 January 1917 and 4 February 1947.
The Great Wass Island Preservation is a open space reserve located on the coast of Maine, east of Ellsworth, Maine on Great Wass Island. The reserve, managed by the land conservation non-profit organization The Nature Conservancy, is notable for its subarctic plants and coastal jackpine.
Based on the Köppen climate classification, this mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Beaver River.
Based on the Köppen climate classification, Mount Galwey is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Galwey drains into tributaries of the Waterton River.
Kalmia microphylla, known as alpine laurel, bog laurel, swamp-laurel, western bog-laurel or western laurel, is a species of Kalmia of the family Ericaceae. It is native to North America and can be found throughout the western US and western and central Canada below the subarctic.
Based on the Köppen climate classification, Mount Watson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Watson drains into tributaries of the Mitchell River.
Parasagitta elegans and the three subspecies occur in Arctic and subarctic waters. S. elegans elegans is a coastal subspecies with oceanic influence. S. elegans arctica is a boreal-arctic form, and S. elegans baltica is the smallest form, found only in or near the Baltic Sea.
Ledum was a genus in the family Ericaceae, including 8 species of evergreen shrubs native to cool temperate and subarctic regions of the Northern Hemisphere and commonly known as Labrador tea. It is now recognised as a subsection of section Rhododendron, subgenus Rhododendron, of the genus Rhododendron.
Based on the Köppen climate classification, Mount Engelhard is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Mount Murray is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather conditions, July to September are best for climbing.
Mt. Christie Based on the Köppen climate classification, Mount Christie is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Christie drains into the Athabasca River.
Based on the Köppen climate classification, Catacombs Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Cinquefoil Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Cinquefoil Mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Curator Mountain is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Curator Mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Mount Crandell is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Crandell drains into Waterton Lake, thence Waterton River.
Based on the Köppen climate classification, Mount Boswell is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Boswell drains into Waterton Lake, thence Waterton River.
Based on the Köppen climate classification, Roche à Bosche is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from Roche à Bosche drains into the Athabasca River.
Based on the Köppen climate classification, Amber Mountain is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Amber Mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, The Whistlers is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from The Whistlers drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Mount Glasgow is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains into the Elbow River which is a tributary of the Bow River.
Based on the Köppen climate classification, Yellowhead Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb.
Isit has a subarctic climate (Köppen climate classification Dfc). Winters are very cold with average temperatures from to in January, while summers are mild with average temperatures from to in July. Precipitation is quite low, but is significantly higher in summer than at other times of the year.
Khoseda-Khardsky has a subarctic climate (Köppen climate classification Dfc). Winters are severely cold with average temperatures from to in January, while summers are mild with average temperatures from to . Precipitation is moderate, and is somewhat higher from July to October than at other times of the year.
Salix herbacea, the dwarf willow, least willow or snowbed willow, is a species of tiny creeping willow (family Salicaceae) adapted to survive in harsh arctic and subarctic environments. Distributed widely in alpine and arctic environments around the North Atlantic Ocean, it is one of the smallest of woody plants.
Retrieved on 2008-04-16. and monthly temperatures which are above for one to three months of the year, with permafrost in large parts of the area due to the cold winters. Winters within subarctic climates usually include up to six months of temperatures averaging below .Susan Woodward.
Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains west into the Illecillewaet River, or east into the Beaver River.
Alcan Border is located at (Sec. 04, T026N, R022E, Copper River Meridian) in the Fairbanks Recording District. It is just inside the Alaska- Canada border, southeast of Northway and northeast of Beaver Creek, Yukon, along the Alaska Highway. Alcan Border has a dry-winter continental subarctic climate (Köppen Dwc).
Based on the Köppen climate classification, Fisher Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb.
Based on the Köppen climate classification, Mount Howard Douglas is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Howard Douglas drains into tributaries of the Bow River.
Based on the Köppen climate classification, Mount Fox is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20° C with wind chill factors below −30° C. In terms of favorable weather, June through September are the best months to climb it.
Based on the Köppen climate classification, Mount Bonney has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains north into the Illecillewaet River, or south into the Incomappleux River.
Based on the Köppen climate classification, Mount Ascension is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes.
Syngrapha ignea, the mountain beauty, is a moth of the family Noctuidae. It is found from northern Alaska south to southern California and New Mexico, with a disjunct population in Labrador. It is also found sparingly across the boreal forest and the subarctic. The wingspan is 29–32 mm.
Pechora has a subarctic climate (Köppen climate classification Dfc). Winters are very cold, with average low temperatures in January of in January. Summers are mild, with average high temperatures in July of . Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Based on the Köppen climate classification, Andy Simons Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes.
Based on the Köppen climate classification, Mount Adair is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes.
Sparwood has a warm-summer humid continental climate (Köppen Dfb) with relatively cold and very snowy winters combined with moderately warm summers with relatively high diurnal temperature variation. As a result of the low overnight lows in summer, September's mean of places Sparwood just above subarctic climates in classification.
Kvæfjord: Strawberries The unique growing conditions, with ripening in 24-hr daylight and modest warmth is sometimes claimed to enhance flavor. Bioforsk, with research in terrestrial effects of climate and subarctic agriculture, has branches in four places in Northern Norway – Tromsø, Bodø, Tjøtta and Svanhovd in Sør-Varanger.
Anadyr experiences a dry-summer subarctic climate (Köppen climate classification: Dsc) according to the Köppen climate classification. Winters are long and very cold; summers are cool and short. January is the coldest month with an average temperature of . July is the warmest month with an average temperature of .
Tarialan has a subarctic climate (Köppen climate classification Dwc) bordering on a humid continental climate (Köppen climate classification Dwb) with mild summers and severely cold winters. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
Based on the Köppen climate classification, Twin Peaks are located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into tributaries of the Knik River.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb.
Based on the Köppen climate classification, the mountain experiences a subarctic climate with cold, snowy winters, and mild summers. The Lake Louise Ski Resort is located to the immediate northwest of the peak. Temperatures can drop below -20 °C with wind chill factors below -30 °C in the winter.
Based on the Köppen climate classification, Mount Patterson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Mount Patterson drains into the Mistaya River which is a tributary of the Saskatchewan River.
Based on the Köppen climate classification, Mount Unwin is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Mount Unwin drains down the Maligne River, which is a tributary of the Athabasca River.
Based on the Köppen climate classification, Eagle Peak has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains west into the Illecillewaet River, or east into the Beaver River.
Lycopodium lagopus (one-cone club-moss) is an arctic and subarctic species of plants in the genus Lycopodium in the clubmoss family. It is widespread in cold, northerly regions: Canada, Greenland, Russia, Scandinavia, and the northern United States including Alaska.Czerepanov, S. K. 1981. Sosudistye Rasteniia SSSR 509 pages.
The lake is in the subarctic climate zone. Average annual precipitation is , of which falls in the spring and summer. Mean annual temperature is , and ranges from in winter to in summer. There are on average 94 days without freezing each year, between June 10 and September 14.
Surgut features a continental subarctic climate (Köppen climate classification Dfc), with long and very cold winters and short but relatively warm summers. Precipitation is moderate, and is higher from May to October, when rain is more frequent, than in the rest of the year, when snow is more frequent.
The city features a subarctic climate (Köppen climate classification: Dfc) with mildly warm summers and very long and cold winters. Precipitation is mostly concentrated between late spring and early fall, peaking in the months of July and August. A freeze has been recorded for every month of the year.
Sovetskaya Gavan has a humid continental climate (Köppen Dfb). The mild September temperatures caused by seasonal lag keep the climate within the continental range. Apart from that there is a strong subarctic and Siberian High influence that keeps winters extremely cold for a coastal location at 49 degrees latitude.
Based on the Köppen climate classification, Cecil Rhode Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes.
Piteå has a climate that is classified as subarctic climate (Köppen climate classification Dfc), bordering to a Humid continental climate (Köppen climate classification Dfb). The warmest months in Piteå are June, July, and August, with high temperatures of . The coldest are December, January, and February, with low temperatures of .
Based on the Köppen climate classification, Kleodora Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Kleodora Peak drains into tributaries of the Athabasca River.
Udachny has an extreme subarctic climate (Köppen climate classification Dfd). Winters are extremely cold, with average temperatures from to in January, while summers are mild, with average temperatures from to in July. Precipitation is quite low, but is significantly higher in summer than at other times of the year.
Aeshna subarctica, the subarctic darner, is a species of darner in the family Aeshnidae. It is found in Europe & Northern Asia (excluding China) and North America. The IUCN conservation status of Aeshna subarctica is "LC", least concern, with no immediate threat to the species' survival. The population is stable.
Kugluktuk is located on the shore of the Arctic Ocean. The surrounding landscape is dominated by the rocky and often barren Canadian Shield. The region has a subarctic climate, but barely so, with July having an average of . It has very cold and extremely dry winters, light snowfall.
Based on the Köppen climate classification, Mount Chester is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb.
Coniferous forests are composed of needle-leaved evergreen trees, such as pine or fir. Evergreen forests are typically found in regions with moderate climates. Boreal forests, however, are an exception as they are found in subarctic regions. Coniferous trees often have an advantage over broadleaf trees in harsher environments.
Millman holds a Ph.D. in Literature from Rutgers University. A fellow of the prestigious Explorers Club, he has made over 30 trips to the Arctic and Subarctic. He has discovered a previously unknown lake in Borneo, and there is a mountain named after him outside Tasiilaq in eastern Greenland.
Betula platyphylla, the Japanese white birch or Siberian silver birch, is a tree species belonging to the genus Betula. It can be found in temperate or subarctic places of Asia: Japan, China, Korea and Siberia. The Japanese White Birch can grow to be 20 m to 30 m tall.
Canadian Journal of Fishery and Aquatic Science, Volume 41, page 1800, 1984. Lake Bienville is on the southern edge of the subarctic climate zone. The lake has an area of 1015 km.2. Freshwater seals have been reported living in the lake, and wood caribou roam around its shores.
In relation to the nearby community of Tatla Lake and indeed the rest of the Chilcotin Plateau off to the east, Tatlayoko Lake tends to be wetter in the winter and drier in the summer. Tatlayoko Lake has a continental climate (Dfb), bordering on a subarctic climate (Dfc).
Evensk has a cold subarctic climate (Köppen climate classification Dfc), with very cold, snowy winters and rather cool, short summers. Precipitation is quite high compared to interior Siberia, and somewhat higher in summer than at other times of the year. Climate data was taken from nearby settlement of Nayakhan.
Grande Cache experiences a subarctic climate (Köppen climate classification Dfc). Summertime is usually very mild, but can also be very cool or warm depending on the movement of different airmasses in the area. Wintertime is very cold and snowy, lasting from November into March, and sometimes even later.
Stolby is located in the East Siberian taiga ecoregion, located in the heart of Siberia. The climate is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ).
The banded gunnel lives in arctic and subarctic waters in the Arctic Ocean, near Southern Labrador and Western Greenland, and in the North Pacific Ocean. It lives in the benthic zone, in sand, broken shells, and gravel. The temperature of the water usually ranges from 5-10 degrees Celsius.
Based on the Köppen climate classification, Mount Crillon has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff and meltwater from its glaciers drains into Glacier Bay and the Gulf of Alaska.
Skovorodino has a subarctic climate (Köppen climate classification Dwc). Winters are severely cold with average temperatures from in January, while summers are mild with average temperatures from in July. Precipitation is moderate and is much higher in summer than at other times of the year. Winters are generally dry.
Based on the Köppen climate classification, Commonwealth Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb.
Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains west into the Illecillewaet River, or east into the Beaver River.
Based on the Köppen climate classification, Mount Charlton is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from Mount Charlton drains into the Maligne River, which is a tributary of the Athabasca River.
The IUCN Red List of Threatened Species. Downloaded on 20 February 2016. It lives in oceans around the world from tropical to subarctic waters. Flashing of photophores of Malacosteus niger, showing red fluorescence modifying the bioluminescence The postorbital photophore in this species is larger than in M. australis.
Based on the Köppen climate classification, Mount Cornwall is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains into the Elbow River which is a tributary of the Bow River.
100px Based on the Köppen climate classification, Mount Coleman is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Coleman drains into tributaries of the North Saskatchewan River.
Based on the Köppen climate classification, Roche de Smet is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Roche de Smet drains into tributaries of the Athabasca River.
This extends the entire range of the northern coast of Ontario with Hudson Bay and James Bay, at which numerous wetlands act as staging and nesting grounds for migratory birds. The waters of the two bays are in the Arctic Archipelago Marine ecozone, forming its southern, subarctic extent.
According to the Köppen Climate Classification Austria has the following climate types: Oceanic (Cfb), Cool/Warm-summer humid continental (Dfb), Subarctic/Subalpine (Dfc), Tundra/Alpine (ET) and Ice-Cap (EF). It is important to note though that Austria may experience very cold, severe winters, but most of the time they are only around as cold as those in somewhat comparable climate zones, for example Southern Scandinavia or Eastern Europe. As well, at higher altitudes, summers are usually considerably cooler than in the valleys/lower altitudes. The subarctic and tundra climates seen around the Alps are much warmer in winter than what is normal elsewhere due in part to the Oceanic influence on this part of Europe.
The climate of Alaska is determined by average temperatures and precipitation received statewide over many years. The extratropical storm track runs along the Aleutian Island chain, across the Alaska Peninsula, and along the coastal area of the Gulf of Alaska which exposes these parts of the state to a large majority of the storms crossing the North Pacific. The climate in Juneau and the southeast panhandle is a mid-latitude oceanic climate (similar to Scotland, or Haida Gwaii), (Köppen Cfb) in the southern sections and a subarctic oceanic climate (Köppen Cfc) in the northern parts. The climate in Southcentral Alaska is a subarctic climate (Köppen Dfc) due to its short, cool summers.
Khabarovsk Krai has a severely continental climate with its northern areas being subarctic with stronger maritime summer moderation in the north. In its southerly areas, especially inland, annual swings are extremely strong, with Khabarovsk itself having hot, wet and humid summers which rapidly transforms into severely cold and long winters, where temperatures hardly ever go above freezing. This is because of the influence of the East Asian monsoon in summer and the bitterly cold Siberian High in winter. The second largest city of Komsomolsk-on-Amur has even more violent temperature swings than Khabarovsk with winter average lows below but in spite of this avoiding being subarctic because of the significant heat in summer.
Olenyok has a subarctic climate (Köppen climate classification Dfc). Winters are extremely cold with average temperatures from in January, while summers are mild with average temperatures from . Temperature of was recorded in January 1959. Precipitation is quite low, but is somewhat higher in summer than at other times of the year.
Each female spawns approximately 350,000 to 3.6 million eggs, depending on their size. Males and females are both presumed to die soon after. Hatchlings are around long and grow rapidly, reaching a length of after a month. The paralarvae migrate northwards toward the waters bordering subarctic regions during summer and autumn.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Rundle drains into the Bow River which is a tributary of the Saskatchewan River.
Wiseman has a continental subarctic climate (Köppen Dfc). Summers are short but mild with rainy days and cool nights. Winters are long and severely cold. Annual snowfall averages 73 inches (185 cm) with peak snow depth occurring during the months of February or March and being 24 inches (61 cm).
Flowering Plant Families of the World. Firefly Books: Ontario, Canada. . The family has a subcosmopolitan distribution, ranging from the subarctic to the southernmost parts of Africa, Australia, and South America. Notable members of the Oleaceae include olive, ash, jasmine, and several popular ornamental plants including privet, forsythia, fringetrees, and lilac.
Based on the Köppen climate classification, Observation Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Observation Peak drains into the Mistaya River, a tributary of the North Saskatchewan River.
Chegdomyn has a monsoon- influenced humid continental/subarctic climate (Köppen Dwb/Dwc) with severely cold, dry winters and very warm, rainy summers. Temperatures in the area of the city typically change by over over the course of the year, with a daily average of in January, compared to in July.
Caecosagitta macrocephala is a deep sea marine chaetognath that is distributed in meso- and bathypelagic layers. It has a very wide distribution that ranges from the Subantarctic to Subarctic Ocean. Miyamoto, H., Machida, R. & Nishida, S. (2010). Genetic diversity and cryptic speciation of the deep-sea chaetognath Caecosagitta macrocephala (Fowler, 1904).
Based on the Köppen climate classification, Radio Control Tower is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, this mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, Mount Foch is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. In terms of favorable weather, June through September are the best months to climb Mount Foch.
The Aleutian tern stands out from its congeners because it is the only species to show an annual migratory behaviour between a subarctic breeding zone and tropical wintering areas in the South Pacific. Only a very small number of Charadriiformes breeding in Alaska appear to have a connection to East Asia.
56 One week after the food drop, all dogs participating in the race undergo a preliminary veterinarian inspection to ensure they are healthy enough to race 1,000 miles in subarctic conditions. Saari, Matias. "Most dogs get the go-ahead at Yukon Quest vet check", Fairbanks Daily News- Miner. February 8, 2009.
Moran experiences a subarctic climate (Dfc) due to its high elevation and aridity, with cold snowy winters, and generally warm summers with nights still dropping to near- freezing temperatures. The data below were compiled from 1911 to when this chart was created (July 2018). They were accessed via the WRCC.
According to the Köppen climate classification system, Gates of the Arctic National Park and Preserve has a Subarctic with Cool Summers and Year Around Rainfall Climate (Dfc). The plant hardiness zone at Anaktuvuk Pass Ranger Station is 2b with an average annual extreme minimum temperature of -42.6 °F (-41.4 °C).
Based on the Köppen climate classification, Mount Amery is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. The months June through August offer the most favorable weather for viewing and climbing this mountain.
Despite lying more than a degree and a half above the Arctic Circle, Dudinka has a subarctic climate (Köppen climate classification Dfc) with short, mild summers and severely cold winters. Precipitation is moderate; it falls mostly as rain in summer and mainly as snow throughout the rest of the year.
Based on the Köppen climate classification, Mt. Dickey is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Bratsk has a subarctic climate (Köppen climate classification Dfc). Winters are very cold and long with average temperatures from to in January, while summers are mild to warm with average temperatures from to in July. Precipitation is moderate and is significantly higher in summer than at other times of the year.
The Great Wass Island Preservation contains heaths and thin acidic soil on coastal bedrock. It is noted for a diverse plant population which includes carnivorous plants, subarctic iris (Iris hookeri), and coastal jackpine (Pinus banksiana). The preserve offers of trails for hiking. An interpretive brochure is provided at the trailhead kiosk.
Chuvanskoye has a continental subarctic climate (Dfc).McKnight and Hess, pp.232–5 The village experiences extremely cold winters. Temperatures generally do not rise above freezing between the beginning of October and the following May and are generally below −20 °C between the beginning of November and the following February.
Based on the Köppen climate classification, Mount Cairnes is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into Blaeberry River which is a tributary of the Columbia River.
The park is in the Carpathian montane forests ecoregion. Because of its altitude, the climate of the Carpathian Park is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1–3 months above ) and cold, snowy winters (coldest month below ).
The Ronald River is the Sept-Rivières Regional County Municipality, Côte-Nord, Québec, Canada. It is in a region with Köppen climate classification Dfc (Subarctic climate). It is a tributary of the Rivière MacDonald, which in turn is a tributary of the Rivière aux Rochers. The river is used by salmon.
Based on the Köppen climate classification, Mount Prince Henry is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, the best months for climbing are July through September.
Last pink alpenglow on Mount Fisher Based on the Köppen climate classification, Mount Fisher has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Kootenay River.
Lasionycta subdita is a moth of the family Noctuidae. It is a subarctic species and is found across Labrador, Quebec and Ontario to Churchill, Manitoba on the west shore of the Hudson Bay. A disjunct population is found in the White Mountains of New Hampshire. Adults are on wing in July.
Based on the Köppen climate classification, Devils Couch has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into Gwillim Creek and Evans Creek, both tributaries of the Slocan River.
Andenes has a climate on the boundary between the subarctic and the subpolar oceanic climates, due to it being extremely mild for its latitude as a result of Gulf Stream influence. Summers are extremely cool due to the moderation, whereas even during the polar night period, daytime highs frequently rise above freezing.
Based on the Köppen climate classification, Archduke Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from its glaciers drains into tributaries of the Duncan River.
Based on the Köppen climate classification, Emperor Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Emperor Peak and meltwater from its glacier drains into tributaries of the Duncan River.
Based on the Köppen climate classification, Midway Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains east to the Mistaya River, or west into tributaries of the Blaeberry River.
Based on the Köppen climate classification, Mount Macduff is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Macduff and meltwater from its surrounding glaciers drains into tributaries of the Duncan River.
Based on the Köppen climate classification, Truce Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from its surrounding glaciers drains into tributaries of the Duncan River.
Based on the Köppen climate classification, Mount Macbeth is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Macbeth and meltwater from its surrounding glaciers drains into tributaries of the Duncan River.
The highlands experiences an Oceanic climate. Winters in Albania are characteristically mild and wet while summers are warm and dry. The northern areas of country such as the Albanian Alps experiences a subarctic climate with frequently very cold winters, and short, mild summers. The lowlands of Albania have mild winters, averaging about .
The "warm-season" cereals are tender and prefer hot weather. Barley and rye are the hardiest cereals, able to overwinter in the subarctic and Siberia. Many cool-season cereals are grown in the tropics. However, some are only grown in cooler highlands, where it ' "may" ' be possible to grow multiple crops per year.
Gonatus is a genus of squid in the family Gonatidae, comprising twelve species, and therefore containing the most species in the family. Adult squid belonging to species in this genus are notable for their lack of tentacles.Diversity, distribution and ecology of gonatid squids in the subarctic Pacific: A review. K. Jefferts, 1983.
This ecoregion is rich in minerals. The climate of Olyokma is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above ) and cold, snowy winters (coldest month below ). Snow begins in October in Olekminsky, and last on average 200 days.
Deputatsky has an extreme subarctic climate (Köppen climate classification Dfc bordering on Dfd). Winters are prolonged and bitterly cold, with up to seven months of sub-zero high temperatures, so that the soil remains permanently frozen. Permafrost and tundra cover most of the region. Average temperatures range from in January to in July.
Based on the Köppen climate classification, Hilda Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Hilda Peak drains east into Hilda Creek, thence Nigel Creek, tributaries of the North Saskatchewan River.
Based on the Köppen climate classification, Portal Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Portal Peak drains into the Bow River which is a tributary of the Saskatchewan River.
Roads may close occasionally during heavy snowfall. Summer temperatures can reach the 80s, but are more often in the mid to high 70s. Combined with mountain breezes, this makes summers refreshing and cool. For being a borderline subarctic climate daytime temperatures are very mild, indicating high diurnal temperature variation due to the altitude.
Based on the Köppen climate classification, Mount Lougheed is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Lougheed drains into the Bow River which is a tributary of the Saskatchewan River.
Based on the Köppen climate classification, Mount Lorette is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into the Kananaskis River which is a tributary of the Bow River.
The Great Plains west of the 100th meridian are semi-arid. Much of the Western mountains have an alpine climate. The climate is arid in the Great Basin, desert in the Southwest, Mediterranean in coastal California, and oceanic in coastal Oregon and Washington and southern Alaska. Most of Alaska is subarctic or polar.
Based on the Köppen climate classification, Pigeon Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Pigeon Mountain drains into the Bow River which is a tributary of the Saskatchewan River.
Poste Montagnais has a subarctic climate (Köppen climate classification Dfc), with long cold winters and short warm summers. The warmest temperature recorded was on June 23, 1989. The coldest temperature recorded was on January 30, 1976. Poste Montagnais has pretty much uniform precipitation throughout the year with slightly more in the summer months.
Based on the Köppen climate classification, Mount Warspite is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River, thence into the Bow River.
Manitoba's northern region is mostly within in the subarctic climate zone (Köppen climate classification Dfc). It also has some Humid Continental (Koppen Dfb) areas in the south. This region features long and extremely cold winters and brief, warm summers with little precipitation. Overnight temperatures as low as occur on several days each winter.
Based on the Köppen climate classification, Little Temple is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Little Temple drains into the Bow River which is a tributary of the Saskatchewan River.
The climate is subarctic. In general, the southern part of the island is warmer, wetter, and windier than the north. The coldest part of the country is the Central Highlands. The low-lying inland areas further north are the driest part but these areas of the country get the heaviest snowfalls in winter.
Based on the Köppen climate classification, Neptuak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Neptuak drains east into tributaries of the Bow River, or west into tributaries of the Vermilion River.
Based on the Köppen climate classification, Mount Fox is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the mountain drains west into the Incomappleux River, or east into the Beaver River.
Based on the Köppen climate classification, Mount McGillivray is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount McGillivray drains into the Bow River which is a tributary of the Saskatchewan River.
The preserve's climate is subarctic at lower elevations, typically up to the timberline at to , and arctic at higher elevations. Winters extend from October to March, with temperatures that occasionally reach . Days are short, with about six hours of light. Summertime highs range between and and exceptional high temperatures of have been recorded.
Based on the Köppen climate classification, Pulpit Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Pulpit Peak drains into the Bow River which is a tributary of the Saskatchewan River.
The geographic area now called Val-Morin was likely inhabited by First Nations people either Montagnais-Naskapi, Algonkin or Cree prior to European settlement.Jenifer S. H. Brown and C. Roderick Wilson (1986). "The Eastern Subarctic - A Regional Overview." In R. Bruce Morrison and C. Roderick Wilson (eds.) Native Peoples The Canadian Experience.
The lowest temperature of was registered in the village of Shtyllë, Librazhd on 9 January 2017. The Albanian Alps in the north enjoy a subarctic climate. Rainfall naturally varies from season to season and from year to year. The country receives most of the precipitation in winter months and less in summer months.
With fruit-crop abundance varying from year to year, pine grosbeak is one of many subarctic- resident bird species that exhibit irruptive behavior. In irruption years, individuals can move long distances in search of suitable food supplies, bringing them farther south and/or downslope than is typical of years with large fruit crops.
Based on the Köppen climate classification, Sunwapta Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Sunwapta Peak drains into the Sunwapta River which is a tributary of the Athabasca River.
Enterprise has a subarctic climate (Dfc) with the yearly mean temperature being below zero in spite of the relatively warm summers around resulting in Enterprise being well below the tree line in the boreal forest. Winter average highs are around with lows being , typical of the boreal forests north of the prairies.
Novy Urengoy has a subarctic climate (Köppen climate classification Dfc). Winters are severely cold and long with average temperatures from to in January, while summers are mild and brief with average temperatures from to in July. Precipitation is moderate, and is somewhat higher in summer than at other times of the year.
Younger specimens, highlighting scaled cap Cortinarius violaceus is found across North America, Europe and Asia. Although widespread, it is not common anywhere in Europe, and it is listed as endangered in the British Isles. Cortinarius violaceus is a rare component of subarctic areas of western Greenland. It has not been recorded from Iceland.
It is much more continental than areas further west on the European continent, with summers characterized by temperatures averaging and lack of precipitation, resembling continental hot-summer mediterranean climates, and subarctic winters with little snow but with chilling temperatures. These vast temperature swings are more comparable to Siberia and the North American plains.
Based on the Köppen climate classification, Bow Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Bow Peak drains into the Bow River which is a tributary of the Saskatchewan River.
The mountain ranges have subarctic and tundra climates. There is also very high rainfall in areas exposed to the Atlantic, such as Bergen. Oslo, in comparison, is dry, being in a rain shadow. Skjåk in Oppland county is also in the rain shadow and is one of the driest places with precipitation annually.
Dawson City has a dry-summer subarctic climate (Köppen climate classification: Dsc), similar to the territory capital of Whitehorse. The average temperature in July is and in January is . The highest temperature ever recorded is on 9 July 1899 and 18 June 1950. The lowest temperature ever recorded is on 3 February 1947.
Nadym experiences a subarctic climate (Köppen climate classification Dfc). The climate is extreme, with temperatures as low as and as high as . On average, however, the region is very cold, with an average temperature of . Precipitation tends to be fairly low; per year, which is heavier in the summer than in the winter.
Wenquan has a tundra climate (Köppen classification ET) bordering very closely on a subarctic climate (Köppen classification Dfc). It has cool summers with some precipitation and cold, dry winters. The yearly precipitation is , which means Wenquan is technically in a desert. Due to its high elevation, there is high diurnal temperature variation.
Many climate zones are found in the ecoregion, due to the altitude zones and geographic surroundings. Typical high elevations exhibit a climate classification of a Tundra or Alpine climate (Köppen climate classification (ET)). Lower elevations trend into a Subarctic climate (Dsc) (mean temperatures may rise above for 1–3 months each summer).
The Taltheilei Shale Tradition is the archeological name of the material culture of a late prehistoric western-area subarctic people dated to the period of 750 BC to AD 1000. The Taltheilei Shale Tradition is named after the "Taltheilei Narrows" (place of open water) of Great Slave Lake. Taltheilei people were Proto-Athapaskans.
Based on the Köppen climate classification, Mount Cairnes is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak and meltwater from its pocket glaciers drains into tributaries of the Kaskawulsh River.
The climate prevailing in the lowland is subarctic and severe, characterized by long, very cold winters. The average temperature in January is by the seashore and inland. In July the average temperature reaches by the seashore, but stays a chilly in the inland zone. Most of the lowland is covered by tundra.
Based on the Köppen climate classification, Hagen Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains west into the Blaeberry River, or east into headwaters of the Amiskwi River.
The border region surrounding Årjäng has a borderline oceanic/continental climate in recent decades, although in previous decades such as the 1961-1990 it was even cold enough to be classified as mild subarctic. The nearest weather station is in Blomskog, located within the woods at a similar altitude somewhat farther south.
Paulatuk has a subarctic climate (Dfc), narrowly avoiding being a tundra climate (ET) due to July having an average temperature above . Rainfall is in limited amounts and confined to the months of June - September because all other months don't have an average temperature above freezing, which would be warm enough for rain.
Peter Baker (1887–1973), born Bedouin Ferran, also known as Ahmad Ali Ferran and Faron Ahmed upon death, was a Lebanese-born Canadian trader, politician, and author. As the first Muslim elected to public office in Canada, he played a fundamental role in the history of Islam in the Arctic and Subarctic regions.
Ust-Omchug has a very cold subarctic climate (Köppen climate classification Dfc). Winters are prolonged and very cold, with up to eight months of sub-zero high temperatures, so that the soil remains permanently frozen. Permafrost and tundra cover most of the region. Average temperatures range from in January to in July.
Based on the Köppen climate classification, Mushroom Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into the Sunwapta River which is a tributary of the Athabasca River.
This research supports decision-making and sustainable development in the Arctic. The multidisciplinary research at the Arctic Centre focuses on the interaction between man and the nature. International research is carried out in the arctic, subarctic and boreal zones. The research builds new multidisciplinary and interdisciplinary practices between natural and social environmental research.
The Alberta–British Columbia foothills forests are a temperate coniferous forests ecoregion of Canada. This ecoregion borders Canada's taiga and contains a mix of subarctic forest and temperate forest species as a result. This makes the region an ecotone region, or a region that acts as a buffer between two other biomes.
Based on the Köppen climate classification, Cone Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Cone Mountain drains into the Bow River which is a tributary of the Saskatchewan River.
Ivittuut holds the record for Greenland's highest recorded temperature of . The lowest recorded temperature was . Ivittuut has a tundra climate (ET) bordering on a subarctic climate (Dfc) with July having an average of 49.6 °F (9.8 °C). Summertime temperatures are cool with chilly nights and wintertime temperatures are very cold with frigid nights.
Based on the Köppen climate classification, Mount Cumnock is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Cumnock drains into Snake Indian River which is a tributary of the Athabasca River.
Taymyr is located in the Taimyr-Central Siberian tundra ecoregion. This ecoregion covers the shore of the White Sea and the Arctic Ocean, including the inlets and islands. The low wetlands are important breeding grounds for waterfowl. The climate of Taymyr is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)).
Based on the Köppen climate classification, Banded Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the mountain drains into the Elbow River which is a tributary of the Bow River.
Based on the Köppen climate classification, Avalanche Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains west into the Illecillewaet River, or east into the Beaver River.
Based on the Köppen climate classification, Peyto Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Peyto Peak drains into the Mistaya River which is a tributary of the Saskatchewan River.
Howse Peak Based on the Köppen climate classification, Howse Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Howse Peak drains into the Mistaya River, Howse River, and the Blaeberry River.
The glen to the west of the summit is a fine example of a parabolic glacial valley Looking north from the summit over the Pass of Drumochter The Sow has several interesting biological specimens on its surface. Phyllodoce caerulea (Norwegian blue heather) is to be found growing on its slopes, this is a subarctic plant which requires steep, partially stabilised block scree slopes and peaty soil. At one time The Sow of Atholl was thought to be only site in the British Isles where Phyllodoce caerulea grew but it has now been located growing in the Ben Alder range as well. Other plants native to subarctic regions such as Cornus suecica (Eurasian dwarf cornel) and Sibbaldia procumbens are to be found on the hill.www.rhb.org.
Based on the Köppen climate classification, Tumbling Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into tributaries of the Vermilion River, or west into headwaters of the Kootenay River.
Based on the Köppen climate classification, Mount Harkin is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into tributaries of the Cross River, or directly west to the Kootenay River.
The 2007 TransSyberia Rally ran from Moscow, Russia to the Mongolian capital of Ulaanbaatar. The 6,600 kilometer route crossed the Ural Mountains, subarctic forests, and the Altai Mountains. The route continued across the Mongolian plains and through the Gobi Desert.Home 25 of 34 entered teams drove Porsche Cayennes – the Porsche Cayenne S Transsyberia Edition.
Based on the Köppen climate classification, Stairway Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains east to the Mistaya River, or west into tributaries of the Blaeberry River.
Based on the Köppen climate classification, Aiguille Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains east to the Mistaya River, or west into tributaries of the Blaeberry River.
Based on the Köppen climate classification, Mount Niles is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Niles drains into the Yoho River and Niles Creek, both tributaries of the Kicking Horse River.
Based on the Köppen climate classification, Mount Vaux is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Vaux drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River.
Based on the Köppen climate classification, The Lieutenants is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into headwaters of Jumbo Creek and Horsethief Creek, both tributaries of the Columbia River.
In Sweden, fjäll refers to any mountain or upland high enough that forest will not naturally survive at the top, in effect a mountain tundra. Fjäll is primarily used to describe mountains in the Nordic countries, but also more generally to describe mountains shaped by massive ice sheets, primarily in Arctic and subarctic regions.
Wrigley has a continental subarctic climate (Dfc). The area combines mild to warm, short summers with long and very cold winters. The differences between the coldest and warmest month are rather extreme even by continental standards, with the January high being and the July high being according to Environment Canada. Transitional seasons are rather short.
Slana experiences a continental subarctic climate (Köppen Dfc), with long, cold winters, and relatively warm summers. Temperature extremes range from . Snowfall averages , with total precipitation of per year. According to the United States Census Bureau, the CDP has a total area of , of which, of it is land and of it (0.37%) is water.
In spite of its maritime position just above the 50th parallel, Havre-Saint-Pierre has a relatively harsh subarctic climate, with cold winters and cool summers, although the fourth-warmest month of September is relatively close to the isotherm to be cold humid continental. The high precipitation brings a lot of snowfall in winter.
Galuut has a subarctic climate (Köppen climate classification Dwc) with mild summers and severely cold winters. The average minimum temperature in January is , and temperatures as low as have been recorded. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
Based on the Köppen climate classification, Cathedral Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Cathedral Mountain drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River.
The summit of Turbacz has a subarctic climate (Köppen Dfc) due to its elevation. The average temperatures are comparable with those found in places in far Northern Europe, such as Alta, Norway, however, the high annual precipitation in combination with the low temperatures places it firmly within the Subalpine Rainforest zone according to Holdridge.
Based on the Köppen climate classification, Mount Huber is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Huber drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River.
Based on the Köppen climate classification, Wiwaxy Peaks is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the peaks drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River.
Borzya has a humid continental climate (Köppen climate classification Dwb) bordering on a subarctic climate (Köppen climate classification Dwc) and a semi-arid climate (Köppen climate classification BSk), with severely cold winters and warm summers. Precipitation is quite low but is somewhat higher from June to September than at other times of the year.
Achinsk has a chilly continental climate (Köppen Dfb) or a slightly warmer subarctic climate (borderline Dfc), just like its neighbouring cities in southern Krasnoyarsk Krai. Winter is moderately cold, just like Siberia, however some ludicrous temperatures of almost minus sixty has been recorded in January 1931. Summer is mildly hot, maybe a little chilly.
Based on the Köppen climate classification, Mount Brett is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Brett drains into tributaries of the Bow River, which is a tributary of the Saskatchewan River.
Based on the Köppen climate classification, Caldron Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from Caldron Peak Peak drains into the Mistaya River which is a tributary of the North Saskatchewan River.
Based on the Köppen climate classification, Mount Peechee is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Peechee drains into tributaries of the Bow River, which is a tributary of the Saskatchewan River.
Based on the Köppen climate classification, Mount Charles Stewart is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Charles Stewart drains into the Bow River which is a tributary of the Saskatchewan River.
Severo-Kurilsk has a subarctic climate (Köppen Dfc). The monthly average temperature is greater than 10 degrees Celsius only in August and September. Due to the influence of the cold current of the Oyashio current , it is cold and humid all year round. The annual precipitation is more than five times that of Siberia.
Tobolsk has a humid continental climate (Köppen climate classification Dfb) bordering on a subarctic climate (Köppen climate classification Dfc). Winters are very cold with average temperatures from to in January, while summers are mild with average temperatures from . Precipitation is moderate and is somewhat higher in summer than at other times of the year.
Farming is a large-scale practice in the temperate regions (except for Boreal/Subarctic regions) due to the plentiful rainfall and warm summers, because most agricultural activity occurs in the spring and summer, cold winters have a small effect on agricultural production. Extreme winters or summers have a huge impact on the productivity of agriculture.
Based on the Köppen climate classification, Mount Tekarra is located in a subarctic climate with long, cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Tekarra drains into the Maligne River and Tekarra Creek, both tributaries of the Athabasca River.
The Japanese common toad, Japanese warty toad or Japanese toad (Bufo japonicus) is a species of toad in the family Bufonidae. It is endemic to Japan. Its natural habitats are subarctic forests, temperate forests, temperate shrubland, swamps, freshwater marshes, intermittent freshwater marshes, freshwater springs, arable land, rural gardens, urban areas, ponds, and irrigated land.
Voss has a subarctic climate, with cold winters and mild summers. It is in the innermost part of the Bolstadsfjorden and includes the valleys that head inland from there. Voss has several large lakes: Evangervatnet, Hamlagrøvatnet, Lønavatnet, Oppheimsvatnet, Torfinnsvatnet, and Vangsvatnet. In the north, Voss reaches to the Nærøydalen valley, which leads to the Nærøyfjorden.
An early summer day at Jewel Lake Park in western Anchorage, Alaska. Anchorage has a subarctic climate (Köppen climate classification: Dfc) but with strong maritime influences that lead to a relatively moderate climate. Most of its precipitation falls in late summer. Average daytime summer temperatures range from approximately ; average daytime winter temperatures are about .
Tosontsengel has a subarctic climate (Köppen climate classification Dwc) with mild summers and bitterly cold winters. The average minimum temperature in January is , and temperatures as low as have been recorded. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
Based on the Köppen climate classification, Mount Lowell is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C. Precipitation runoff from Mount Lowell drains into Fryatt Creek and Lick Creek, both tributaries of the Athabasca River.
Khanty-Mansiysk experiences a subarctic climate (Köppen climate classification Dfc). The climate is extreme, with temperatures as low as and as high as . On average, however, the region is very cold, with an average temperature of . Precipitation tends to be fairly low; per year, which is heavier in the summer than in the winter.
Based on the Köppen climate classification, Franchère Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Franchère Peak drains into Portal Creek and Astoria River which are both tributaries of the Athabasca River.
The climate of Kalevalsky is Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc)). This climate is characterized by mild summers (only 1–3 months above ) and cold, snowy winters (coldest month below ). The number of days with snow cover is 170-180; the number of frost-free days is 80–95 days.
The Nuu- chah-nulth of Vancouver Island began whaling with advanced long spears at about this time. The Maritime Archaic is one group of North America's Archaic culture of sea-mammal hunters in the subarctic. They prospered from approximately 7,000 BCE–1,500 BCE (9,000–3,500 years ago) along the Atlantic Coast of North America.
Based on the Köppen climate classification, Mount Jimmy Simpson is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Jimmy Simpson drains into the Bow River which is a tributary of the Saskatchewan River.
Renchinlkhümbe has a subarctic climate (Köppen climate classification Dwc) with cool summers and bitterly cold winters. The average minimum temperature in January is , and temperatures as low as have been recorded. Most precipitation falls in the summer as rain, with some snow in the adjacent months of May and September. Winters are very dry.
Based on the Köppen climate classification, Mount Hurd is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Hurd drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River.
Based on the Köppen climate classification, Mount Cooper has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from the Spokane Glacier drains east into Cooper Creek, a tributary of the Duncan River.
La Ronge experiences a borderline subarctic climate (Köppen Dfc), slightly below the threshold of a humid continental climate. Winters are long, dry and very cold while summer is short, warm and wetter. Precipitation is low, with an annual average of 486.2 mm. The highest temperature ever recorded in La Ronge was on 23 August 1929.
Based on the Köppen climate classification, Mount Poland is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into Blaeberry River and Waitabit Creek, which are both tributaries of the Columbia River.
Trisetum is a genus of plants in the grass family, widespread in temperate, subarctic, and alpine habitats in much of the world.Persoon, Christiaan Hendrik. 1805. Synopsis Plantarum 1: 97-98 in LatinGrassbase - The World Online Grass FloraFlora of China Vol. 22 Page 325 三毛草属 san mao cao shu Trisetum Persoon, Syn.
Due to Edson's high elevation, the community experiences a subarctic climate (Köppen climate classification Dfc). The highest temperature ever recorded in Edson was on 2 July 1924. The coldest temperature ever recorded was on 22 January 1943, and 14 January 1950. Summers in Edson are generally mild to warm with chilly nights and moderate precipitation.
Strategies for revegetation of disturbed gravel areas in climate stressed subarctic environments with special reference to Churchill, Manitoba, Canada: A literature review. Climate Research 5 49-52. The Inuit have many names for the species, including malikkaat, isuqtannguat, isurramuat, and piluit. They monitored the status of the plant in order to track the seasons.
Based on the Köppen climate classification, Xerxes Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20° C with wind chill factors below -30° C. Precipitation runoff from Xerxes Peak drains into Fryatt Creek and Lick Creek, both tributaries of the Athabasca River.
Based on the Köppen climate classification, Karpathos Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20° C with wind chill factors below -30° C. Precipitation runoff from Karpathos Peak drains into Fryatt Creek and Lick Creek, both tributaries of the Athabasca River.
Based on the Köppen climate classification, Mount Birdwood is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the mountain drains into tributaries of the Spray River which is a tributary of the Bow River.
Based on the Köppen climate classification, Dragon Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C. Precipitation runoff from Dragon Peak drains into Fryatt Creek and Luck Creek, both tributaries of the Athabasca River.
M. maorum is commonly found in the waters of New Zealand and South Australia. preferring temperate to subarctic waters. In New Zealand they are found off the coasts of both the North and South islands. M. maorum is also common in the waters of the islands surrounding New Zealand including Campbell, Chatham and Auckland islands.
Based on the Köppen climate classification, Opal Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Opal Peak drains west into the Maligne River which is a tributary of the Athabasca River.
Stordalen mire (elevation 351 m) lies in the subarctic region in northernmost Sweden. It is located 10 km east of the town of Abisko close to Lake Torneträsk. It is a 25 ha palsa mire, which is common in the discontinuous permafrost zone. The mire has two major topographical features: elevated palsas and depressions.
Based on the Köppen climate classification, Devils Couch has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from the New Denver Glacier on the north slope drains into tributaries of the Slocan River.
Based on the Köppen climate classification, Mount Moffit is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. This climate supports the Trident Glacier surrounding this peak. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, Matanuska Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into tributaries of the Matanuska River, which in turn is a tributary of the Knik River.
Based on the Köppen climate classification, Redoubt Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Redoubt Peak drains into the Athabasca River on its east side, and the Fraser River from the west side.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, July and August present the best months for climbing. However, these months coincide with mosquito season, which requires effective defenses.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, July and August present the best months for climbing. However, these months coincide with mosquito season, which requires effective defenses.
Köppen-Geiger climate classification classifies its climate as subarctic (Dfc). Between 1961 and 1990 Samedan had an average of 95.5 days of rain per year and on average received of precipitation. The wettest month was August during which time Samedan received an average of of precipitation. During this month there was precipitation for an average of 11.5 days.
Based on the Köppen climate classification, Mount Drysdale is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into tributaries of the Vermilion River, or west into tributaries of the Beaverfoot River.
The climate of this region is mostly Subarctic climate, without dry season (Köppen climate classification Subartic climate (Dfc and Dsc)). This climate is characterized by mild or cool summers (only 1–3 months above ) and cold, snowy winters (coldest month below ). with oceanic influences. There is no permafrost south of 57 degrees north, reflecting the relatively warmer conditions.
Based on the Köppen climate classification, Mount Sifton is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from surrounding glaciers on its slopes drains into tributaries of the Beaver River and Illecillewaet River.
Tolerance to sand burial, trampling, and drought of two subarctic coastal plant species (Leymus mollis and Trisetum spicatum). Arctic, 418-428. Fungal disease resistance: In addition to these tolerance factors, Leymus mollis is also resistant to many fungal diseases. One example of this tolerance is with wheat stripe rust, a plant infection caused by Puccinia striiformis.
Based on the Köppen climate classification, Eyebrow Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Eyebrow Peak and meltwater from its surrounding glaciers drains into Horsethief Creek, which is a tributary of the Columbia River.
Saint-Prime has a humid continental climate that is some way above the subarctic classification due to its warm summers. Winters, however, are very cold and the seasonal differences are severe, although not extreme by Canadian or Quebec standards. Precipitation levels are high, bringing much snowfall in winter, but are by no means extreme compared to adjacent areas.
Mayo has the warmest summers in the Yukon with a mean average summer temperature of . Mayo has a subarctic climate (Koppen: Dfc), with generally warm summers and severely cold winters lasting half the year. Spring and autumn are very short transitional seasons between summer and winter, with average temperatures rising and falling very fast during these times.
Based on the Köppen climate classification, Morro Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Morro Peak flows into the Athabasca River.
Marbleton has a subarctic climate (Koppen: Dfc), with generally warm, sometimes hot summers, and brutally cold and long winters. Diurnal temperature range is very high all year round, but even more so during summertime, with August having an average daily temperature range of 42 degrees Fahrenheit (23.3 Celsius). The nearest offivcial weather station is in nearby Big Piney.
Yerbogachen has a subarctic climate (Köppen climate classification Dfc). Winters are bitterly cold with average temperatures from to in January, while summers are warm with average temperatures from to . Precipitation is quite low, but is significantly higher in summer than at other times of the year. Yerbogachen has a climate comparable to that of the Yakutia.
These open areas can include those such as coastal dunes, other coastal spots, lakeshores, islands, moorlands, steppes, meadows, prairies, other extensive grasslands and rather shrubby areas of the Subarctic. These may be favored due to their vague similarity to the flat openness of the tundra.Fuller, M., Holt, D. & Schueck, L. (2003). Snowy Owl movements: Variation on the migration theme.
Kotlik is located at . Kotlik is located on the east bank of the Kotlik Slough, 35 miles northeast of Emmonak in the Yukon-Kuskokwim Delta. According to the United States Census Bureau, the city has a total area of , of which, of it is land and of it (17.85%) is water. The climate of Kotlik is subarctic.
It lies at approximately 64.333890° North Latitude and -161.153890° West Longitude. (Sec. 23, T013S, R013W, Kateel River Meridian.) Shaktoolik has a subarctic climate with maritime influences when Norton Sound is ice-free, usually from May to October. Summer temperatures average 47 to 62; winter temperatures average -4 to 11. Extremes from -50 to 87 have been recorded.
As it is not near the ocean, this area is drier than coastal Alaska and experiences seasonal extremes typical of subarctic areas. The annual precipitation is only 12 inches (305 mm), including 37 inches (94 cm) of snow. The average low temperature in January is −11 °F (−23 °C). The average high during July is +69 °F (+20 °C).
Denali Park has a subarctic climate (Dfc) like most of Alaska. Summer days are mild with nights being brisk. Winters are severely cold with extremely heavy annual snowfall averaging 79.5 inches (202 cm), with peak snow depth reaching 20 inches (50.8 cm) during March. Most of Denali Park's precipitation occurs during the months of June - September.
Based on the Köppen climate classification, Mount Earl Grey is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of Toby Creek, which in turn is a tributary of the Columbia River.
Assyrians are the indigenous peoples of Northern Iraq. Ethnic groups are abundant throughout Asia, with adaptations to the climate zones of Asia, which can be the Arctic, subarctic, temperate, subtropical or tropical. The ethnic groups have adapted to mountains, deserts, grasslands, and forests. On the coasts of Asia, the ethnic groups have adopted various methods of harvest and transport.
Based on the Köppen climate classification, McHugh Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the peak drains into McHugh, Potter, and Rabbit Creeks, which empty into Turnagain Arm three miles from the summit.
Chapais has a marginal subarctic climate (Koppen: Dfc) just a shade colder than the humid continental (Koppen: Dfb) areas to the south. Winters are bitterly cold, but summers are relatively warm during daytime, but nights remain relatively cool. As such the yearly mean is just above freezing. Summers have high rainfall and winters are quite snowy.
Rim Village. During the winter, the road up to Rim Village is normally plowed but Rim Drive is closed. According to the Köppen climate classification system, Crater Lake National Park has a continental subarctic climate - Cold Dry Summer (Dsc). The plant hardiness zone at the lake is 6b with an average annual extreme minimum air temperature of .
Olyokminsk has a subarctic climate (Köppen climate classification Dfc). Winters have temperatures averaging from in January, while summers have average temperatures from in July. In the summer months of June, July, and August, it is not uncommon for temperatures to surpass during the day. Precipitation is significantly higher in summer than at other times of the year.
Smithers has a borderline humid continental/subarctic climate (Köppen climate classification Dfb/Dfc). Winters are cold and cloudy but highly variable with a January average of . Snow is the main type of precipitation during winter. Warm spells can push temperatures above freezing during the winter months, while cold weather systems can reduce the temperature to less than .
In subarctic areas, Empetrum has been a vital addition to the diet of the Inuit and the Sami. After waning popularity, the crowberry is regaining its reputation as an edible berry. It provides a steady crop and the gathering is relatively easy. The high concentration of anthocyanin pigment can be used as a natural food dye.
Based on the Köppen climate classification, Rearguard Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from the mountain drains into the Robson River.
Based on the Köppen climate classification, Hewitt Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into Numa Creek, a tributary of the Vermilion River, or west into tributaries of the Kootenay River.
The Holarctic Drosophila populi species group belongs to the subgenus Sophophora and contains two species, Drosophila ingrica and Drosophila populi. D. ingrica is found in the Palearctic, while D. populi is found in the Nearctic. Both species are found in the northernmost subarctic forest zone, and are strongly associated with cottonwood trees.Vilela, C. R., and G. Bächli. 2009.
Based on the Köppen climate classification, Mount Goode is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Knik Glacier which surrounds the mountain. The months May through June offer the most favorable weather for climbing.
"Phylogenetic Systematics of the Genus Mertensia (Boraginaceae)". Systematic Botany 39(1):268-303. . Notable exceptions are Mertensia maritima, a maritime plant of Arctic and subarctic coastlines, and Mertensia virginica, which is found from the Appalachian Mountains west to Minnesota, Iowa, and Missouri. Most of the species are endemic to very small areas of the Rocky Mountains.
Based on the Köppen climate classification, Roche Miette is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Roche Miette drains into the Athabasca River.
The Anishinaabe are a group of culturally-related Indigenous peoples resident in what are now Canada and the United States. They also include the Odawa, Saulteaux, Ojibwe (including Mississaugas), Potawatomi, Oji-Cree, and Algonquin peoples. The Anishinaabe speak Anishinaabemowin, or Anishinaabe languages that belong to the Algonquian language family. They historically lived in the Northeast Woodlands and Subarctic.
Heceta Bank's ocean currents and dynamics are similar to that of the entire Oregon coast. Along the Oregon coast, the California Current is the major Pacific Ocean Current. It runs southward, bringing colder subarctic water down along the West Coast. The Davidson Current is a coastal counter-current that runs northward along the inside of the California Current.
Schefferville has a subarctic climate (Köppen Dfc). Schefferville has cool summers relative to its latitude and inland location. The cold winters are caused in part by elevation, and in part the ice cover of Hudson Bay eliminating maritime moderation in winter. Although Schefferville is nearer the Atlantic, the cold Labrador Current brings cold air also from the east.
The forest types are mainly subarctic (boreal) and cool-temperate forest. Pinus densiflora dominates coniferous forests across North Korea, and has also increased in abundance in areas altered by human impact. The main botanic garden in North Korea is the Central Botanical Garden, established in 1959. It is located at the base of Mount Taesong in Pyongyang.
The suppliers of "dead wood" emphasise its age: the wood has developed with dehydration in the dry coldness of the subarctic zones, the tree having stopped growing after some 300–400 years, and the tree has remained upright for another few hundred years. "Dead wood" logs are easier to transport and handle than normal logs due to their lightness.
Based on the Köppen climate classification, Mount James Walker is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into the Kananaskis River which is a tributary of the Bow River, and thence the Saskatchewan River.
Never Cry Wolf is an account of the author's experience observing wolves in subarctic Canada by Farley Mowat, first published in 1963 by McClelland and Stewart. It was adapted into a film of the same name in 1983. It has been credited for dramatically changing the public image of the wolf to a more positive one.
The Hokkaidō deciduous forests ecoregion (WWF ID:PA0423) covers the northern and southern coasts of the island of Hokkaido, the northernmost of the main islands of Japan. The region sits in the transition zone between the colder subarctic forests to the north and the more temperate forests to the south. Characteristic trees include Mongolian oak, Basswood, and Ash trees.
Based on the Köppen climate classification, Mount Sarbach is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Sarbach drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.
The tail is white with a dark terminal band. The feet are feathered. The rough-legged buzzard (Buteo lagopus), also called the rough-legged hawk, is a medium-large bird of prey. It is found in Arctic and Subarctic regions of North America, Europe and Russia and the Palearctic during the breeding season and migrates south for the winter.
Members of this order are mostly pelagic fishes living in deep oceanic waters. Their distribution around the world's oceans is very wide, ranging from subtropical and temperate waters up to subarctic or even Antarctic ones. FishBase (2005), Nelson (2006): p.207 Head of Sloane's Viperfish, Chauliodus sloani The smallest species of this order is the bristlemouth Cyclothone pygmaeae.
Umiat has a subarctic climate with long winters. February is the coldest month, a common trait on the North Slope, and average temperatures remain below 0°F until mid-April. Severe cold can persist well into spring; on April 5, 1995, the temperature fell to −50°F. Precipitation is irregular and snow has occurred in every month but July.
As a Siberian town, Severobaikalsk experiences a subarctic climate, characterized by extreme variation of temperatures between seasons. Temperatures can be very warm in the summer, and brutally cold in the winter. The warmest month of the year in Severobaikalsk is July, when the mean temperature is . The coldest month of the year is January, when the mean temperature is .
Based on the Köppen climate classification, Epaulette Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Epaulette Mountain drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.
Reindeer herds form the basis of pastoral agriculture for several Arctic and Subarctic peoples. Pastoralism involves managing domesticated animals. In nomadic pastoralism, herds of livestock are moved from place to place in search of pasture, fodder, and water. This type of farming is practised in arid and semi-arid regions of Sahara, Central Asia and some parts of India.
Banff experiences a subarctic climate (Köppen climate classification Dfc) that borders on a humid continental climate (Köppen Dfb). Winter temperatures range from an average low of to an average high of . Summer temperatures in the warmest month are an average high of and an average low of . Snow has been recorded in all months of the year.
Based on the Köppen climate classification, Kaufmann Peaks is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Kaufmann Peaks drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.
Dulce is the southernmost urban area with a subarctic humid continental climate in North America (Köppen: Dfc) where summer is mild and short due to high altitude and rigorous winter. Going further south than the Dfb in low altitude and in latitude similar to the southern limit of the Dfa in the center of the country.
Irkutsk originally had a borderline subarctic climate (Köppen climate classification Dwc). Since 2000, the temperatures have resembled a humid continental climate (Köppen climate classification Dwb). Snow cover has disappeared earlier, from late April in the 1930s to late March in the 1980s. Discontinuous permafrost depth had decreased from 200 m to 100 m during the same period.
Delsbo has historically had a transitional climate between humid continental and subarctic. Recent warming has put Delsbo firmly within the continental zone, with four months of the year being above in mean temperatures. Summers are very warm for the northerly latitude in combination with quite moderate winters, that still retains larger seasonal differences than nearby Hudiksvall.
Based on the Köppen climate classification, White Pyramid is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from White Pyramid drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.
While Plains and Plateau tribes are renowned for their beaded horse trappings, Subarctic tribes such as the Dene create lavish beaded floral dog blankets.Berlo and Philips, p. 151 Eastern tribes have a completely different beadwork aesthetic: Innu, Mi'kmaq, Penobscot, and Haudenosaunee tribes are known for symmetrical scroll motifs in white beads, called the "double curve."Berlo and Phillips, p.
In 1929, he (and Pat Reid) made the first midwinter flight to Hudson Bay. He was also involved in formation of several airlines, including Oaks Airways Ltd. He participated in several lifesaving mercy flights, including a search and rescue flight of 13 prospectors stranded in the subarctic. In later years, he settled into being a mining analyst in Toronto.
Based on the Köppen climate classification, Mount Paul is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Paul drains west into Maligne Lake, thence into the Maligne River which is a tributary of the Athabasca River.
The park was formalized as a National Park in 2013. The park is spread over two districts on the Chukchi Peninsula: Providensky District to the south, and Chukotsky District to the north. The topography is maritime highland subarctic tundra. The mountains are medium height – averaging 900 meters, with the highest being Mt. Iskhodnaya at 1194 meters.
Based on the Köppen climate classification, Samson Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Samson Peak drains west into Maligne Lake, thence into the Maligne River which is a tributary of the Athabasca River.
Based on the Köppen climate classification, Leah Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Leah Peak drains west into Maligne Lake, thence into the Maligne River which is a tributary of the Athabasca River.
Fort Smith has a dry continental subarctic climate (Koppen: Dfc) with very long winters combined with warm but relatively short summers. The highest temperature ever recorded in Fort Smith was on July 18, 1941. The coldest temperature ever recorded was on 26 December 1917. These are both the hottest and coldest temperatures ever recorded in the Northwest Territories.
Bironico has a Continental Subarctic climate (Dfc) under the Köppen climate classification. The average annual temperature is . The average coldest month was January with an average temperature of , while the warmest month was July with an average temperature of . The wettest month was May during which time Bironico received an average of of rain or snow.
Jasper experiences a borderline Humid Continental/Subarctic climate (Köppen climate classification Dfb/Dfc). The highest temperature ever recorded in Jasper was on 16 July 1941. The coldest temperature ever recorded was on 24 January 1916. Summers in Jasper are pleasant, with daily highs usually around 70 °F (21.1 °C) and lows around 45 °F (7.2 °C).
Based on the Köppen climate classification, Mount Abbe has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Clark, Johns Hopkins, and Gilman Glaciers on its slopes. Precipitation runoff and meltwater from its hanging glaciers drains into Johns Hopkins Inlet.
Trondheim Airport Værnes is used as the official meteorological office for this region. Temperatures in both the winter and summer are moderate due to the geography of the location: the average January highs are still above freezing despite a high latitude. Hell has a humid continental climate that is close to being subarctic and also close to being oceanic.
Altai has a typical Mongolian cold semi-arid climate (Köppen BSk) with subarctic (Dfc) influences, although the climate is so dry as to qualify as semi-arid despite the annual mean being sufficient for sporadic permafrost. The climate experiences long, very dry and very cold winters with short, mild summers when the majority of the scant precipitation occurs.
Hammerfest has a subarctic climate (Köppen climate classification Dfc). In spite of the extreme northern location, there is no permafrost, as the mean annual temperature is approximately , about the same as Anchorage, Alaska which is located at a latitude of 61° North. Monthly 24-hr averages range from in January to in July. Mean annual precipitation is .
The Chipewyan subsequently became important in the subarctic trade by exchanging furs and hides for metal tools, guns, and cloth. Modern Chipewyan are either fluidly sedentary or semi-nomadic in lifestyle. Many still practice their traditional lifestyle for subsistence like fishing or hunting caribou although this process is modernized with the use of modern nets, tools, transportation and more.
The Taiga Shield Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is an ecozone which stretches across Canada's subarctic region. Some regions exhibit exposed Precambrian bedrock of the Canadian Shield, the oldest of the world's geological formations. The world's oldest rocks, dating to four billion years, are found in the Canadian Shield north of Great Slave Lake.
A rock glacier descends from the cirque to the lake. A steep five kilometre trail provides access to the amphitheatre, and an additional three kilometres on a beaten path reaches the summit via the east ridge. Based on the Köppen climate classification, Kings Throne Peak is located in a subarctic climate with long, cold, snowy winters, and mild summers.
Egvekinot has a subarctic climate (Köppen Dfc) falling just short of a tundra climate (Köppen ET). Temperatures can be below freezing from October all the way through to the following May, and below from December through to March. The short summer is temperate. The average temperature in January is , and the average temperature in July is .
Vilhelmina has a subarctic climate that is less severe than typical for a far inland locality at this latitude, but still very cold by Swedish standards. Its higher altitude causes summers to be cooler than coastal areas like Skellefteå further east, whereas winters are somewhat tempered by maritime air from the greater Atlantic and the North Atlantic Current.
Based on the Köppen climate classification, Yukness Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Yukness Mountain drains into Lake O'Hara, thence into the Kicking Horse River which is a tributary of the Columbia River.
Ust-Ilimsk has a subarctic climate (Köppen Dfc) with warm, humid summers and severely cold, drier winters. The monthly 24-hour average temperature ranges from in January to . Precipitation is moderate and is somewhat higher in summer than at other times of the year. Sunshine is generous and the area receives 2,011 hours of bright sunshine annually.
Based on the Köppen climate classification, Silverhorn Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Silverhorn Mountain drains west into the Mistaya River, or east into Dolomite Creek which is a tributary of the Siffleur River.
Bironico has a Continental Subarctic climate (Dfc) under the Köppen climate classification. The average annual temperature is . The average coldest month was January with an average temperature of , while the warmest month was July with an average temperature of . The wettest month was May during which time Bironico received an average of of rain or snow.
Fire cycles also tend to be long near the tree line in the subarctic spruce-lichen woodlands. The longest cycles, possibly 300 years, probably occur in the western boreal in floodplain white spruce. Amiro et al. (2001) calculated the mean fire cycle for the period 1980 to 1999 in the Canadian boreal forest (including taiga) at 126 years.
Based on the Köppen climate classification, Watermelon Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Watermelon Peak drains into the Bow River and Siffleur River which are both tributaries of the Saskatchewan River.
Fort Providence has a continental subarctic climate (Dfc) typical of the Northwest Territories' populated areas. It is marked by a long cold winter season and short, warm summers, that in many ways are warmer than expected for an area so far north. Transition seasons are extremely short, with temperatures rising and falling quickly in respective seasons.
Based on the Köppen climate classification, Oubliette Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, July and August present the best months for climbing. However, these months coincide with mosquito season, which requires effective defenses.
Upon the Canadian Shield and in the coolest weather, are subarctic lichen woodland. The black spruce (Picea Mariana), jack pine (Pinus banksiana), and white spruce (Picea glauca) are commonly occurring trees. This area is interspersed with peatlands, bogs, fens, permafrost areas, and areas of arctic tundra. Yellow and Grey Reindeer moss (Cladonia mitis) provide ground cover.
Dease Lake has a subarctic climate (Dfc), typical of northern British Columbia. Summers are mild, coupled with chilly nights while winters are severely cold and snowy, with annual snowfall averaging 84 inches (213 cm). Autumn typically begins by early September and lasts into October where Winter begins. Winter can last into late March or sometimes early April.
Based on the Köppen climate classification, Mont des Poilus is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mont des Poilus drains into the Yoho River and Amiskwi River, both tributaries of the Kicking Horse River.
Based on the Köppen climate classification, The Castelets is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from The Castelets drains into the Alexandra River.
Based on the Köppen climate classification, Coronach Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Coronach Mountain drains into tributaries of the Snake Indian River, which in turn is a tributary of the Athabasca River.
Based on the Köppen climate classification, Mount Colin is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Mount Colin flows into the Athabasca River.
Based on the Köppen climate classification, Mount Bogart is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into the Kananaskis River and west into Spray Lakes Reservoir which both empty to the Bow River.
Based on the Köppen climate classification, Gargoyle Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Gargoyle Mountain flows into the Athabasca River.
The long winter causes about half of the annual precipitation in the north to fall as snow. Precipitation in the south amounts to about annually. Like that of the north, it occurs all through the year, though not so much of it is snow. In Köppen climate classification Finland belongs to the Df group (continental subarctic or boreal climates).
He began his career in research of body-fossils and trace fossils in the eastern part of the Czech Cretaceous Basin. In his publications promotes for the region the term "podorlická křída". Since 2008, he studies the fossil assemblages in the Arctic and Subarctic region.Leita eftir spor-steinrenningum frá ístíðini og kanna Hg-innihaldið í føroyskum gróti.
The plant life of the reserve is that of wet subarctic coniferous forest. Dominant trees are spruce and fir, with some larch forests. The treeless areas are sometimes called "tundra" for some physical resemblance to true tundra, by in fact contain extensive peat bogs up to 6 meters thick. Characteristic plants are sedges, grasses, and plants with underground runners.
Based on the Köppen climate classification, Mount Outram is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from Mount Outram drains into tributaries of the Howse River.
Based on the Köppen climate classification, Hawk Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Hawk Mountain flows into the Athabasca River.
Based on the Köppen climate classification, Esplanade Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Esplanade Mountain flows into the Athabasca River.
Based on the Köppen climate classification, Floe Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into Floe Creek, a tributary of the Vermilion River, or west into tributaries of the Kootenay River.
Terrace Bay has a humid continental climate (Koppen: Dfb), bordering on a subarctic climate (Koppen: Dfc) with September having an average of only 1.8 F (1 C) more than the 50 degree isotherm used to determine subarctic climates. Summers are very mild due to the moderation of nearby Lake Superior, with the warmest month, August, only having an average high of 68.4 degrees Fahrenheit (20.2 c). Winters are long, cold, and snowy, averaging 83 inches (211 cm) of snow per year. Terrace Bay shows signs of seasonal lag, with August being warmer on average than July, likely due to the towns proximity to Lake Superior, which causes towns on the lake influenced by the lake, to take longer to warm up than towns not on or near the lake.
Remarkably for its relatively southerly latitude, Kurilsk has a humid continental climate (Köppen Dfb) that almost qualifies as a subarctic climate owing to the powerful influence of the cold Oyashio Current which makes summers exceptionally cool. Unlike most subarctic climates, however, the winters are fairly mild and there is no permafrost. Precipitation, as with all the Kuril Islands, is very heavy owing to the influence of the Aleutian Low, though Kurilsk is a little less wet than Yuzhno-Kurilsk because of its westerly aspect which tends to shelter it from cyclonic storms originating over the Pacific. The climate actually resembles the subpolar oceanic climate of the Aleutian Islands more than the climate of interior Siberia, but the mean February temperature of is well beyond the threshold of oceanic climates.
Rosa × alba plants are tall shrubs with arching stems and bluish-green leaves. They bloom only in mid summer. They are extremely cold hardy and disease resistant, hence they are used to create new varieties for subarctic climates like northern Scandinavia and Canada. These magnificent shrubs can withstand shade and semishade, and are easily found abandoned in semi wild situations.
The reserve is one of the wettest and coldest parts of Belgium. It is frequently shrouded in mist and low cloud. It has a subalpine climate with strong winds and fierce winters, which are occasionally subarctic. The Fagnes plateau intercepts clouds brought by the prevailing Atlantic winds, and this results in copious precipitation, with an average of of rain per year.
Drunken trees, tilted trees, or a drunken forest, is a stand of trees displaced from their normal vertical alignment. This most commonly occurs in northern subarctic taiga forests of black spruce (Picea mariana) under which discontinuous permafrost or ice wedges have melted, causing trees to tilt at various angles. A drunken forest in Siberia caused by melting permafrost. NASA photo.
The waterfowl genus Anser includes all grey geese (and sometimes the white geese). It belongs to the true geese and swan subfamily (Anserinae). The genus has a Holarctic distribution, with at least one species breeding in any open, wet habitats in the subarctic and cool temperate regions of the Northern Hemisphere in summer. Some also breed further south, reaching into warm temperate regions.
Mount Gray seen from Tumbling Creek Trail Based on the Köppen climate classification, Mount Gray is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into tributaries of the Vermilion River, or west into tributaries of the Beaverfoot River.
Junsele has a subarctic climate with large seasonal and diurnal variations. Summers are short and warm, sometimes very warm during July. Winters are extensive but less severe than in other parts of the world at such a northerly inland latitude. Cold extremes can be severe at times, with an all-time low of during a severe January 1987 cold wave.
According to the Köppen climate classification system, Kenai Fjords National Park has a Subarctic climate (Dfc) with cool summers and year around precipitation. According to the United States Department of Agriculture, the Plant Hardiness zone at Exit Glacier Visitor Center at 463 ft (141 m) elevation is 4b with an average annual extreme minimum temperature of -20.3 °F (-29.1 °C).
Based on the Köppen climate classification, Bastion Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Bastion Peak drains into tributaries of the Athabasca River on its east side, and tributaries of the Fraser River from the west side.
Based on the Köppen climate classification, Grizzly Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from a small unnamed glacier on its northwest slope drains into tributaries of the Beaver River and Illecillewaet River.
Based on the Köppen climate classification, Ursus Minor Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from a small unnamed glacier on its north slope drains into tributaries of the Illecillewaet River and Beaver River.
Based on the Köppen climate classification, Sheep Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing. Precipitation runoff from the mountain drains into tributaries of the Matanuska River.
Based on the Köppen climate classification, Ursus Major Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from small unnamed glaciers on its slopes drains into tributaries of the Illecillewaet River and Beaver River.
Rockhopper penguins are present at a variety of climates and locations; Amsterdam Island's subtropical waters, Kerguelen Archipelago's subarctic coastal waters, and Crozet Archipelago's subantarctic coastal waters. Due to the species plasticity they are able to express different strategies and foraging behaviors depending on the climate and environment. A main factor that has influenced the species' behavior is where food is located.
Based on the Köppen climate classification, Tombstone Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb Tombstone Mountain. Precipitation runoff from the mountain drains into tributaries of the Elbow River.
Fire takes place about 10 weeks after the events of the first novel. It follows the same fantasy like the first and further develops themes of horror fiction, psychological realism and an unreliable narrator(s). The plot also makes analogies to the effects of global warming on Sweden's subarctic climate and the group behaviour dynamics of political, religious and ideological extremist groups.
Based on the Köppen climate classification, Mist Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb Mist Mountain. Precipitation runoff from the mountain drains into tributaries of the Highwood River.
According to the Köppen climate classification system, Denali National Park has a subarctic climate with cool summers (Dfc). The plant hardiness zone at Denali Visitor Center is 3a with an average annual extreme minimum temperature of -38.9 °F (-39.4 °C). Long winters are followed by short growing seasons. Eighty percent of the bird population returns after cold months, raising their young.
Veronica wormskjoldii is a species of flowering plant in the plantain family known by the common name American alpine speedwell. It is native to much of northern and western North America, including the western United States and northern Canada, from where it grows in moist alpine habitat, such as mountain forest understory. It has a wide subarctic distribution from Alaska to Greenland.
Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb the mountain. Precipitation runoff from the mountain drains into tributaries of the Bow River.
Bethel has a subarctic climate (Köppen Dfc), with long, somewhat snowy, and moderately cold winters, and short, mild summers. Normal monthly mean temperatures range from in January to in July, with an annual mean of . Warm days of above can be expected on 14 days per summer. Precipitation is both most frequent and greatest during the summer months, averaging per year.
The climate of Petersburg is a subpolar oceanic climate (Cfc), closely bordering a subarctic climate (Dfc). On January 16, 1981, Petersburg registered a daily maximum temperature of , the highest ever recorded in the month of January in Alaska. Eleven years later, on February 27, 1992, a high of was observed, also setting a monthly state record high. A view of the Petersburg waterfront.
Salix lanata, the woolly willow, is a subarctic species of willow native to Iceland, the Faeroes, northern Scandinavia, Finland, through to eastern Siberia. In Scotland it can be found in only a few localities of Perthshire, Angus and Aberdeen, generally on rocky mountain sides at altitudes between .Willows and Poplars of Great Britain and Ireland, BSBI Handbook No. 4; Meikle; 1984.
Like most of Yukon, Beaver Creek has a subarctic climate (Dfc), and NRC Plant Hardiness Zone of 0a. It is situated at an elevation of approximately . Beaver Creek experiences annual temperature average daily highs of in July and average daily lows of in January. Record high temperature was on June 15, 1969 and the lowest was on January 17, 1971.
Tammisto forest nature reserve Vantaa has a humid continental climate (Köppen: Dfb), slightly above the threshold for subarctic classification. Although the city no longer (since 2009) has a coastline along the Baltic Sea, it is close enough to experience the mitigating influence of the sea and the Gulf Stream. The record low temperature in Vantaa is and the record high is .
Based on the Köppen climate classification, Mount Jellicoe is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb. Precipitation runoff from the mountain drains into headwaters of the Upper Kananaskis River.
New navigator to explore the subarctic waters: The Icebreaking Supply Vessel Gennadiy Nevelskoy delivered at Arctech Helsinki Shipyard. Arctech Helsinki Shipyard, 3 March 2017. On 7 July 2014, the Finnish newspaper Turun Sanomat reported that Arctech Helsinki Shipyard had been awarded the construction of three icebreaking standby vessels for Sovcomflot.Helsingin telakka on saanut kolmen jäänmurtajan tilauksen. Turun Sanomat, 11 July 2014.
Amanita nivalis grows in subarctic and alpine conditions in Europe and also in Greenland. It is often associated with low growing willows (Salix spp.) and birches (Betula spp.). There have been reports of it occurring at high altitudes in the Rocky Mountains in North America. The fruit bodies appear singly or in small groups in both silicaceous and limestone areas in summer.
Tornio has a subarctic climate (Dfc) that is slightly tempered in winter by its proximity to the sea, but retains warm continental summers that are quite short. The weatherbox is from neighbouring city Haparanda and operated by Swedish Meteorological and Hydrological Institute. Despite the fact that Tornio experiences polar day between 15 and 27 June (13 days) it does not experience polar night.
Bonavista has a subarctic climate (Dfc) due to its cold water temperatures surrounding the location, keeping June temperatures below in terms of mean temperatures. Although winters are relatively mild by Canadian standards, there is heavy snowfall and frequent cold days. Winter lasts from December through April. Bonavista is one of the windiest places in Canada with an average wind speed of .
Based on the Köppen climate classification, Mount Sarrail is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20° C with wind chill factors below −30° C. In terms of favorable weather, June through September are the best months to climb Mount Sarrail. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.
The white geese are a small group of waterfowl which are united in the genus or subgenus Chen, in the true geese and swan subfamily Anserinae. They breed on subarctic areas of North America and around the Bering Strait, migrating south in winter. Most authorities now place these species in the grey goose genus Anser. Indeed, Chen and Anser are anatomically indistinguishable.
Based on the Köppen climate classification, Mount Benson is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes. The months May and June offer the most favorable weather for viewing.
The grey-headed chickadee or Siberian tit (Poecile cinctus, formerly Parus cinctus) is a passerine bird in the tit family Paridae. It is a widespread resident breeder throughout subarctic Scandinavia and the northern Palearctic, and also into North America in Alaska and the far northwest of Canada. It is a conifer specialist. It is resident, and most birds do not migrate.
Based on the Köppen climate classification, Resurrection Peaks are located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes. The months May and June offer the most favorable weather for viewing.
Aliserkovo has a Continental Subarctic climate (Dfc). The climate around the settlement is bitterly cold for most of the year, with temperatures below freezing from the end of September and remaining so until the following May. July is the warmest month, with an average daily temperature of 12.6 °C. January is the coldest month, with a mean daily temperature of -48.2 °C.
Based on the Köppen climate classification, Mount Louis is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Weather conditions during summer months are optimum for climbing. Precipitation runoff from Mount Louis drains into the Bow River which is a tributary of the Saskatchewan River.
Based on the Köppen climate classification, Threepoint Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through October are the best months to climb. Precipitation runoff from the mountain drains into tributaries of the Elbow River.
It reaches maturity at in length and specimens from the Arctic and subarctic, which grow to the largest size, can reach up to . The fish has a squat appearance, a large spiny head and a tapering body. It is a mottled grey-brown in colour but can be darker, including black as base coloring. It has a large mouth and spiny gill covers.
235 Before its construction, transportation to Dawson City required a steamboat trip on the Yukon River during the brief subarctic summer, or dog sleds after the rivers had frozen.Killick, p. 57 Abbot, Downing's Overland Wagon After its construction, horse-drawn stagecoach routes soon were established. Even with this regulated travel, it took five days to travel the distance between the two towns.
Based on the Köppen climate classification, Endless Chain Ridge is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Endless Chain Ridge drains west to the Sunwapta River, or east into the Maligne River, both of which are tributaries of the Athabasca River.
Based on the Köppen climate classification, Bullard Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Mendenhall Glacier to the mountain's west. The month of July offers the most favorable weather for viewing and climbing this peak.
Based on the Köppen climate classification, Hogback Ridge is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Corbin, Keystone, and Hogback Glaciers on the mountain. The months May through June offer the most favorable weather for viewing and climbing.
Based on the Köppen climate classification, The Watchtower is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into Excelsior Creek and Watchtower Creek, both tributaries of the Maligne River which in turn empties into the Athabasca River.
Based on the Köppen climate classification, Mount King George is located in a subarctic climate zone with cold, snowy winters, and mild summers. This climate supports the King George Glacier on the eastern slope of the mountain. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Palliser River.
Based on the Köppen climate classification, Mount Bridgland is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, July through September are the best months to climb. Precipitation runoff from the mountain drains into tributaries of the Miette River.
View from the river bank Old Crow has a subarctic climate (Köppen climate classification Dfc) with mild summers and severely cold winters. Average annual temperature is . Old Crow experiences annual temperature average daily highs of in July and average daily lows of in January. Record high temperature was on August 30, 1976 and the lowest was on January 5, 1975.
Based on the Köppen climate classification, McGinnis Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Mendenhall Glacier and Juneau Icefield to the mountain's east. May and June are the best months for climbing in terms of catching favorable weather.
Based on the Köppen climate classification, Utopia Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from Utopia Mountain drains into tributaries of the Athabasca River.
Based on the Köppen climate classification, Mount Fitzwilliam is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for viewing and climbing this mountain. Precipitation runoff from the mountain drains into tributaries of the Fraser River.
Mt. Swanzy Based on the Köppen climate classification, Mount Swanzy is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain and meltwater from the surrounding glaciers drains north into the Illecillewaet River, or south into the Incomappleux River.
Since phytoplankton grow most abundantly along the edges of the ice pack, the concentration of this sulfur-containing organic compounds and their geochemistry provide indicators of how far the ice edge extended from the continent. There are further extensive sets of multicentury historical records of arctic and subarctic sea ice and uses, among others high-resolution paleo proxy sea-ice records.
Manning has a subarctic climate, very close to being a humid continental climate, with both May and September averaging only fractionally under . There are vast differences between the warm summers and very cold winters, although areas much further south more eastward in Canada have equally cold winters and cooler summers. The climate data is from minor settlement Notikewin very close to the town.
Cherepovets has distinctive four-seasons humid continental climate (just above subarctic), with warm summers and cold but not extremely cold winters by Russian standards. It falls into the humid continental zone by the fourth warmest month being just above in mean temperature and the annual temperature being , above the freezing point. Winter, however, lasts for five months, rendering transitional periods rather short.
Based on the Köppen climate classification, Mount Mather is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into the Tanana River drainage basin. The months May through June offer the most favorable weather for climbing or viewing.
Erigeron eriocalyx is a Eurasian species of flowering plants in the daisy family. The species is a widespread flower species in the arctic, subarctic, alpine and subalpine meadows in Russia, Kazakhstan, Mongolia, Inner Mongolia, and Xinjiang.Panarctic Flora, 860713 Erigeron eriocalyx (Ledeb.) Vierh. Erigeron eriocalyx is a perennial, clump-forming herb up to 25 cm (10 inches) tall, forming a branching underground caudex.
Based on the Köppen climate classification, Nigel Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Nigel Peak drains south into the North Saskatchewan River, and north into the Sunwapta River which is a tributary of the Athabasca River.
The azure tit (Cyanistes cyanus) is a passerine bird in the tit family Paridae. It is a widespread and common resident breeder throughout Russia and Central Asia and northwest China, Manchuria and Pakistan. Eggs, Museum Wiesbaden Collection It is found in temperate and subarctic deciduous or mixed woodlands, scrub and marshes. It is resident, and most birds do not migrate.
Based on the Köppen climate classification, it is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.
Xainza has an extreme subarctic climate, bordering on polar. The climate of the county is typical of a plateau climate zone, with thin, cold air and a dry climate, with 279.1 days of frost per year on average. The average annual wind speed is 3.8 m/s (12.5 ft/s), the average annual temperature is , and the average annual precipitation is .
Norman Wells has a subarctic climate (Köppen Dfc) with summer lasting for about three months. Although winter temperatures are usually below freezing, every month of the year has seen temperatures above . Rainfall averages and snowfall . On average, there are 92.9 days, October to April, when the wind chill is below -30, which indicates that frostbite may occur within 10 – 30 minutes.
Kuopio falls in the subarctic climate zone (Köppen "Dfc"), closely bordering on continental due to its warm summers. Winters are long and cold, with average highs staying below freezing from November until March, and summers are short and relatively mild. Most precipitation occurs in the late summer and early fall. The summers are relatively warm for its latitude, especially the lows.
Prince Albert experiences a humid continental climate (Köppen: Dfb). It is close to being subarctic (Dfc) with May and September mean temperatures being just above . The coldest month on average is January with an average low of , and July is the hottest month with an average high of . The highest temperature ever recorded in Prince Albert was on July 19, 1941.
Palana has a subarctic climate (Köppen Dfc), intermediate between those of the Sakha Republic and the eastern coast of the Kamchatka Peninsula. The Sea of Okhotsk freezes during the winter and thus there is less moderation of temperatures during this season than is found on the Pacific side of the peninsula, and the Aleutian Low tends to produce less precipitation.
Based on the Köppen climate classification, Cantata Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. May and June are the best months for climbing in terms of catching favorable weather. Precipitation runoff from the peak drains into tributaries of Eagle River.
Hierochloe is a genus of plants in the grass family known generally as sweetgrass.Brown, Robert. 1810. Prodromus Florae Novae Hollandiae 208-209 in Latin These are perennial rhizomatous grasses found primarily in temperate and subarctic regions of Eurasia and North America, although some species extend southwards into Australia and Latin America.USDA Plants Profile These erect green grasses are known for their sweet scent.
Luetkea is a genus of herbaceous plants in the family Rosaceae. One species is accepted. Luetkea pectinata (partridgefoot or luetkea) is a mat-forming semi- shrub. It is endemic to the cold portions of western North America occurring in subarctic Alaska, Yukon, western Northwest Territories, and subalpine to alpine regions of British Columbia, southwestern Alberta, Washington, Oregon, Idaho, northern California and western Montana.
Based on the Köppen climate classification, Gunsight Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing. Precipitation runoff from the mountain drains into tributaries of the Matanuska River.
Based on the Köppen climate classification, Mount Hayes is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports glaciers on its slopes including the Hayes Glacier. Precipitation runoff from the mountain drains into tributaries of the Tanana River drainage basin.
Based on the Köppen climate classification, Mount Abdallah has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Romer Glacier on the east slopes, and an unnamed glacier on the north flank. Precipitation runoff and meltwater from its glaciers drains into Glacier Bay Basin.
Located in the Cordillera Climatic Region, it lies at the southern end of a subarctic climate (Köppen Dfc). In the summer, the city is often dusty and arid; temperatures during the day are warm, but cool at night, typically falling below . Highs reaching occur only twice per year on average. Heavy rain showers are sporadic, lasting only a few minutes.
Lieksa has a subarctic climate (Köppen: Dfc) with more continental characteristics than most of Scandinavia, making it prone to extreme temperatures, especially in winter. In summer temperatures regularly exceed , and the highest temperature ever recorded was in July 1934. Also, during the Heatwave of 2010, the temperature in Lieksa reached degrees. In winter, the snow cover is usually around 60 cm deep.
The high subarctic forest-tundra of northwestern Canada: position, width, and vegetation gradients in relation to climate. Arctic 45:1-9. The species migrates mainly through tallgrass prairies to winter in open woodlands, woodland edges and clearings, hedgerows, dense riparian thickets and around brush piles. The Harris's sparrow regularly occurs at feeders in suburban and rural gardens during the wintertime.
Kedgwick has a humid continental climate (Dfb) and once had a subarctic climate (Dfc). Summer consists of warm days and cool nights with about half of all days experiencing rain. Winter consists of cold days and frigid nights below zero with extremely heavy annual snowfall averaging 103 inches (261 cm). Kedgwick is one of the coldest and snowiest inhabited places in New Brunswick.
Based on the Köppen climate classification, Mount Erebus is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . This climate supports the Fraser Glacier on the northwest slope, and the Eremite Glacier on the northeast slope. In terms of favorable weather, July and August present the best months for climbing.
Based on the Köppen climate classification, McGinnis Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. This climate supports the Trident, Black Rapids, and McGinnis Glaciers surrounding this peak. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, Mount Shand is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. This climate supports the Trident and Black Rapids Glaciers surrounding this peak. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
In Fennoscandia the range extends almost to the Arctic Circle, as well as in northern Russia. The species is very cold tolerant and lives in a variety of habitats, from forests to open grasslands, from the lowlands up to above the tree line. From temperate areas to the subarctic tundra. The species rises up to 1800 m in the Alps.
Based on the Köppen climate classification, Mount Marathon is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a spruce and hemlock forest on the lower slopes. The months May and June offer the most favorable weather for viewing.
Based on the Köppen climate classification, Hess Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Gillam and West Fork Glaciers surrounding this peak. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, Moby Dick is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. This climate supports the Trident, Susitna, and Black Rapids Glaciers surrounding this peak. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing.
Based on the Köppen climate classification, Mount Macpherson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Despite the modest elevation, the climate supports a small pocket glacier on the northeast face. Precipitation runoff from Mount Macpherson drains north into tributaries of the Columbia River.
Because of its high elevation and mid-continental location, the ecoregion's climate is Subarctic climate, dry winter (Köppen climate classification Subartic climate(Dwc)). This climate is characterized by mild summers (only 1–3 months above ) and cold winters having monthly precipitation less than one-tenth of the wettest summer month. The average temperatures range from in January, and in July.
Based on the Köppen climate classification, Gregorio Peak has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into Gwillim Creek and Hoder Creek, both tributaries of the Slocan River. Its nearest higher peak is Lucifer Peak, to the north-northeast.
Mount Erasmus Based on the Köppen climate classification, Mount Erasmus is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from Mount Erasmus drains into tributaries of the North Saskatchewan River.
Based on the Köppen climate classification, Old Baldy is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.
Based on the Köppen climate classification, Mount Nagishlamina is located in a subarctic climate zone, with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Harpoon and Capps Glaciers surrounding the peak. Precipitation runoff from the mountain and meltwater from its glaciers empties into Cook Inlet.
The genus Atriplex is distributed nearly worldwide from subtropical to temperate and to subarctic regions. Most species-rich are Australia, North America, South America and Eurasia. Many species are halophytes and are adapted to dry environments with salty soils. The genus evolved in Middle Miocene, the C4-photosynthesis pathway developed about 14.1-10.9 million years ago, when the climate became increasingly dry.
The largest volcano in Eurasia – Kluchevskaya (altitude ). With the volcanic activity associated with the formation of many minerals, as well as a manifestation of hydro geo thermal activity: education fumaroles, geysers, hot springs, etc. Despite Kamchatka lying at similar latitudes to Scotland, it is mostly subarctic, more continental in the hinterland and more maritime and prone to monsoons on the coast.
Based on the Köppen climate classification, Mount Black Prince is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . In terms of favorable weather, July through September are the best months to climb. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River, thence into the Bow River.
Based on the Köppen climate classification, Foster Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains east into Floe Creek and Numa Creek which are both tributaries of the Vermilion River, or west into tributaries of the Kootenay River.
In spite of its temperate latitude, the powerful Oyashio Current on the western flank of the Aleutian Low gives Simushir a chilly and very wet subarctic climate (Köppen Dfc) that amazingly almost qualifies as a polar climate (ET), which in low-lying areas would be expected only at latitudes about 20 degrees or further north. Unlike typical subarctic or polar climates, however, the winters are only moderately severe and there is no permafrost since the mean annual temperature is around , whilst temperatures have never fallen below . However, the extreme winds, which in winter average as much as , make it feel much colder.OSTROV SIMUSHIR, RUSSIA Summers are mild, but extraordinarily cloudy with fogs occurring on six-sevenths of all days in summer and annual sunshine hours less than 1,100 per year, which is comparable to Reykjavík or the extremely foggy Sichuan Basin.
As a result, population cycles tend to be found in northern temperate and subarctic ecosystems because the food webs are simpler. The snowshoe hare-lynx system is subarctic, but even this involves other predators, including coyotes, goshawks and great horned owls, and the cycle is reinforced by variations in the food available to the hares. A range of mathematical models have been developed by relaxing the assumptions made in the Lotka-Volterra model; these variously allow animals to have geographic distributions, or to migrate; to have differences between individuals, such as sexes and an age structure, so that only some individuals reproduce; to live in a varying environment, such as with changing seasons; and analysing the interactions of more than just two species at once. Such models predict widely differing and often chaotic predator-prey population dynamics.
Many tribes throughout North America, besides those on the Plains, also painted hides, following different aesthetic traditions. Subarctic tribes are known for their painted caribou hides. On the Plains, when buffalo herds were being slaughtered in the late 19th century, other painting surfaces became available, such as muslin, paper, and canvas, giving birth to Ledger art.Szabo, 16 Contemporary Plains beadwork and jewelry used designs from hide painting.
To the north from Mount Recheshnoi, in the valley of Geyser Creek are located geothermal fields with geysers. In 1988 here were active 5 geysers up to 2 m high and 9 natural fountains up to 0.7 m high. Umnak has a subarctic climate (Köppen: Dfc), which borders on a subpolar oceanic climate (Köppen: Cfc) with short, mild to warm summers and long, cold, snowy winters.
Tampere has a typical subarctic climate (Köppen climate classification Dfc) at the Tampere–Pirkkala Airport (TMP) with only 3 months above , bordering on a warm-summer humid continental climate (Köppen climate classification Dfb). Winters are cold and the average temperature from November to March is below . Summers are cool to warm. On average, snow cover lasts 4–5 months from late November to early April.

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