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336 Sentences With "be wet"

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

type: All Declarative Interrogative Exclamative

structure: All Simple Compound Complex Compound-Complex

length: All <=10 words 10-20 words 20-30 words 30-50 words

"  "Vaginas are built to stretch, they're built to be wet.
Be prepared for changing weather and be prepared to be wet.
The work would be wet and messy, so they wore waders.
Saturday will likely be wet as well, but Sunday's looking splendid.
The Southeast won't just be wet -- it'll also be unusually warm.
These are going to be wet kisses so, get down with it.
"Zaferia used to be wet when Long Beach was dry," he said.
The mixture should be wet but not runny; add a bit of water if needed.
It can be wet and you can walk out the door and it looks good.
The trustees, sticking to temple rules, had insisted that her clothes be wet before entering.
Your dough will be wet, hard to shape and will likely flatten out during baking.
In those days, the uniforms were wool, and after a game they'd be wet with sweat.
"The suspect's shirt that he was wearing appeared to be wet with sweat," the report claims.
Tuesday will be wet and chilly ☔️ There's a chance of rain mostly after 9 a.m.
But then one day, someone's hands happened to be wet and the air knife dried them brilliantly.
" You can go in your normal clothes too, though the spokesperson warns that everything "will be wet.
Many times by the end of the day his pants would be wet because he would piss himself.
Now that early harvests can be wet or dry, drought is no longer a good predictor of wine quality.
"I'm going to be wet now, cause they've started to water the field," he said, as translated by Sputnik News.
I've seen writers and Yelpers and various internet trolls complain about Neapolitan pizzas being wet, but they're to be wet.
There will be wet periods and dry periods — it's just that in both, there will be less water to work with.
Many core growing areas continued to be wet into the start of this year's summer crop planting campaign, slowing the pace.
The Northeast will also be wet, Garrett said, with rain moving through the region in the morning but drying out later.
"If you're heading to the beach for the holiday weekend, it could be wet and windy (with) dangerous surf conditions," he said.
But the Airwrap needs your hair to be wet to work its magic, since it styles with warm (and then cool) wind.
One thing's for certain, though: It will be wet, it will be gory, and, judging by that sex scene, it will be on fire.
They don't really understand what death is and wonder if their loved one is going to be wet and cold if it's raining on his grave.
Accuweather suggests that voters in the Greensboro, North Carolina; Roanoke, Virginia; and Harrisburg, Pennsylvania areas vote in the afternoon, since the morning is expected to be wet.
After the tomatoes have marinated for about 20 minutes, they'll get battered, and since they'll be wet with buttermilk anyway, there's no need for eggs before dredging.
As a matter of fact, my pants are still soaked and the problem is that I feel like my balls are gonna be wet for the next four hours.
"I have actually trained my body and my mind to endure hard things, to be pushing super hard, to be uncomfortable, to be wet, to be cold," O'Brady told Insider.
On top of advanced motion detection and weather-resistant cameras, you get 2-way audio through your smartphone to give instructions for deliveries or scare away would-be Wet Bandits.
When ENSO is in its positive phase, drought can be expected in parts of southern Africa and eastern Brazil, too, while the southern United States can expect things to be wet.
Either way, by day's end they would be wet, tired, hungry and cold: the four pillars of misery the Army has long relied on to help whip recruits into cohesive fighting teams.
Yet despite all this, Lake Mead's users have been overdrawing water in recent years — essentially assuming that there will be wet years in the future to provide surplus water and recharge the system.
Conditions will be wet, but temperatures will be mild in much of the Southeast -- in the 60s and 70s -- and in the 40s in the Northeast as New Year's Eve revelers welcome 2019.
Or animals are trying to haul out (of the water), but people are trying to push or coax them back in because they think that they need to be wet or in water all the time.
For a demographic as young and diverse as that of Highland Park, however, this means that even a simple roast beef sandwich will contain things like yuzu kosho, and the pastrami will be wet-brined and more corned beef-like.
Lenore Correia, a meteorologist with the National Weather Service in Boston, said the snow would be wet and sticky, especially along the coast and in southeast Massachusetts, making driving conditions worse and increasing the likelihood of felled trees, downed power lines and power failures.
It was all wet, which is why I assume it was a boat and not an old-tyme hotel that happened to be wet... but logic informs that it was a sinking ship because the water was ankle deep and my clothes were wet and my hair was wet.
"The concern would be, if you do lose power, the cold's going to be pretty significant Sunday night and Monday," Mr. Schroeter said, adding that he was not expecting major power failures in his area, because the snow was unlikely to be wet and heavy enough to bring down trees.
Then, just when you get comfortable in the format, it skews off and gets more porny: They have competitions like "blow-offs," where the losers are voted out of the house; they have a lineup of pneumatic porn actors saying, "I want my panties to be wet at the end of this competition"; there are a lot of leather sofas with sweat stains on them.
Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
16 Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Ross distributed a smooth basecoat of thinned paint, usually white, along the canvas before painting started so the canvas would always be wet and the pigments could more efficiently mix.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or hiking Jackita Ridge.
The other technique requires the paper to be wet and tamped into the engravings without a paste.Perkins, Dorothy. “stone rubbings, Chinese.” Encyclopedia of China: The Essential Reference to China, Its History and Culture.
16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing the peaks of Elija Ridge.
Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
The shaper material should be non-reactive with both the melt and growth atmosphere, and should be wet by the melt. It is possible to grow multiple crystals from a single crucible using the EFG technique, for example by growing many parallel sheets.
Bideford has a wet but mild climate; during the winter Bideford experiences a lot of frosty nights and mornings and also gets some snow. During the summer Bideford can be wet, but also mild. The Torridge Bridge in Bideford, surrounded by snow.
Most ceramics are extremely hard and must be wet-sawed with a circular blade embedded with diamond particles. A metallography or lapidary saw equipped with a low-density diamond blade is usually suitable. The blade must be cooled by a continuous liquid spray.
Outside of summer, the weather may be wet and cold, and butts may obstruct views of the cliff. The ship stops at several small docks on the way in and out, including a layover at the end of the Lysefjorden at the village of Lysebotn.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy.
Spring and fall are transitional seasons that feature mild weather that can often be wet and unpredictable. There are, on average, 2523 hours of sunshine per year, ranging from a low of 111.6 hours in December to a high of 350.3 hours in July.
A pool party "Wetlook" describes the appearance of fabric which is shiny and thus appears to be wet. It may also describe the act of getting wet while wearing clothes, and enjoyment of doing so or of watching others do so, as a form of sexual excitement.
Klingon does not have adjectives as a distinct part of speech. Instead, many intransitive verbs can be used as adjectives, in which case they follow the noun they modify. Contrast (`wep` coat, and `yIQ` be wet) : `wep yIQ` : the wet coat with : `yIQ wep.` : The coat is wet.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The North Cascades Highway east of Washington Pass has the distinction of being among the top areas in the United State for most avalanche paths per mile of highway.Avalanche Control.wsdot.wa.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
All captains complained of the class's poor stowage capacity, the result of their fine French underwater lines, but stowage improved after the introduction of iron fresh-water tanks. Lastly, captains considered the class to be "wet", a result of lively rolling and pitching causing seams to loosen.Gardiner, pp. 141-142.
Steep cliffs inside river valleys require a certain level of rock-climbing skills. However, because of the humid environment inside river valleys, some rock surfaces can be wet and some rocks may be loose despite appearing solid. To deal with wet climbing conditions, professional river-trekking boots are strongly advised.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
It has two pronounced seasons - the dry and the wet seasons with a temperature coldest at and warmest at . There are 2 seasons for Tublay, Benguet will be wet season from May to October and dry season from November to April. The municipality is located north of Manila and north of Baguio.
16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. This climate supports the Forbidden Glacier in the northwest cirque, the immense Boston Glacier to the east, and glacial remnants on the south side in Boston Basin. These glaciers carved Forbidden Peak into a classic horn.
Buckeye rot is favored by warm, wet weather. Temperatures between are ideal for the fruit rot. In order for sporangia to be produced, allowing the pathogen to reproduce, the soil must be wet and above . Zoospores can only disseminate by swimming in water, so excessive rain and irrigation promote growth of the disease.
The area has been called Mathaysana (11th century) and later Mataisine (13th century) and Mattacena (14th century), which could possibly be derived from Matta ("to be wet") and Cena ("plateau"). This depicts actually rather well both the geography and the climatic characteristics of the place. The inhabitants of Matheysine are called Matheysins.
Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
This might led to development of variants with slightly altered tastes to accommodate regional preferences. Other ethnic groups in Indonesia also have adopted a version of rendang into their daily diet. For example, in Java, the rendang—aside from the Padang variety sold in Padang restaurants—tend to be wet, slightly sweeter and less spicy to accommodate Javanese tastes.
After having tried to involve Jordy in TV advertisements for nappies where the baby should repeat "hard, hard to be wet", Claude Lemoine, Jordy's father, had the idea of using dance music and simple lyrics to create a catchy song. The result was well received in discothèques, which convinced Lemoine to release it as a commercial single.
The weather on the Wednesday the matches were held turned out to be wet and windy. The first Semi Final between Wallaroo and University was entirely one-sided with Wallaroo dominating the scoring. The second Semi Final ended in a fiasco. Ten minutes into the game, a Sydney player was ordered off the field for striking an opponent.
Masuria has a temperate climate with cold winters and warm summers. The weather here is generally a bit cooler than in most parts of Poland, and the area usually experiences several snowfalls during the winter. The Masurian lakes are oftentimes frozen from December until the end of February. Springtime can be wet, while summers are generally drier.
The use of any lubricating powder in crokinole is controversial, with some purists reviling the practice. Powder is used to ensure pieces slide smoothly on the surface. According to carrom rules, the powder must be of high quality to keep the surface smooth and dry, and shall not be wet. Pouches and containers are used to spread the powder over the playing surface.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. Precipitation runoff from the mountain drains into the Hamma Hamma River and Skokomish River.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from Mount Arriva drains into tributaries of the Stehekin and Skagit Rivers.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Normal copy paper with weights of 70–90 g/m2 (19–24 lb) can be used for simple folds, such as the crane and waterbomb. Heavier weight papers of 100 g/m2 (approx. 25 lb) or more can be wet-folded. This technique allows for a more rounded sculpting of the model, which becomes rigid and sturdy when it is dry.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from Indecision Peak drains into tributaries of the Stehekin and Skagit Rivers.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. The months July through September offer the most favorable weather for climbing Mount Walkinshaw.
Ernst Alfred Philippson, Germanisches Heidentum bei den Angelsachsen (1929), p. 104 ("Als männlicher Personenname ist Sunna nach Searles Onomasticon selten ..." However, a 1937 theory held that "The meaning of sunna is likely to be wet or marshy land...[as] in Sonning, h[undre]d. and par[ish] ... near Reading, and in Sunninghill in south-east Berkshire".Robert Eugen Zachrisson, Studia neophilologica, Vols.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from Sluiskin Mountain drains into tributaries of the White River.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from The Tooth drains into tributaries of the Snoqualmie River.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from the mountain drains into the Skagit River.
Snow accumulation sustains the Silver Star Glacier on the north slope of the mountain. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
In the end it is young Swan who knocks Marty out and the trio escape out the front door. The money is found to be wet, gone to mush and therefore completely useless. Jessie and Willis have not broken any laws and are free to go. Just as Marty is dragged away, Jeffrey pulls a gun of his own, and accuses him of sleeping with Lydia.
Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing and climbing this mountain.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
Over fifty different types of birds have been sighted there. It is located north of the town and comprises a reserve of 13 hectares. As it was once part of the Koo Wee Rup Swamp it can often be wet underfoot, particularly during spring time. The sanctuary is home to animals such as frogs, lizards, snakes and water birds and is a rare reserve in this district.
A hadith in Abu Dawud () says: > The Prophet said: There is no prophet between me and him, that is, Isa. He > will descend (to the earth). When you see him, recognise him: a man of > medium height, reddish fair, wearing two light yellow garments, looking as > if drops were falling down from his head though it will not be wet. He will > fight the people for the cause of Islam.
240 mounted in casemates on the sides of the hull underneath the main guns. Their positions tended to be wet in heavy seas, especially the rear guns. These guns could depress to −5 degrees and had a maximum elevation of +20 degrees; they had a rate of fire of six shots per minute. They could fire a high-explosive projectile with a muzzle velocity of to a maximum distance of .
Spores come into contact with healthy leaf and stem tissue of Dianthus plants through wind, rain, and contact with infected tissue. The host plant must be wet or moist for spores to germinate. Moderate to high humidity is also a requirement, and one study found that spores would not germinate under 55% humidity. The life cycle takes about four days from germination to the production of new conidia.
To the northeast of Lake Sterling there is about a of glacial rock and ponds, originally called Glacier Lakes Basin Trails. The trail system usually follows watercourses and is prone to be wet after rain, requiring detours. The trails cross many many marsh areas as well. There are two marked trail systems, red and blue, accessible by crossing the dam, and staying to the right around a helipad.
A stable flat surface and towels are standard. Fibres that tolerate water well may be wet blocked, shaping moist fabric into the desired shape and then allowing it to air dry. Cold blocking uses no heat and less water to achieve the same result by spraying water upon the material instead of immersing the fabric. Steam blocking uses a steamer or steam iron, but without applying direct pressure to the item.
Nymph fishing may be more productive, but dry fly anglers can become addicted to the surface strike. Once a fish has been caught and landed, the fly may be wet and no longer float well. Flies can sometimes be dried by "false" casting back and forth in the air. With care, a small piece of reusable absorbent towel, an amadou patch or a Chamois leather may be used.
Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. In terms of favorable weather, June to October are the best months for hiking up the mountain.Mount Jupiter on Climbersguideolympics.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Homoeomeria was a doctrine in the philosophy of the ancient Greek Anaxagoras, as claimed by the Roman atomist Lucretius.Monica R. Gale, Oxford Readings in Lucretius, 2007, page 139. It was assumed that the atoms constituting a substance must themselves have the salient observed properties of that substance: so atoms of water would be wet, atoms of iron would be hard, atoms of wool would be soft, etc. This doctrine depends on the fallacy of division.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
The gene product is involved in the proper assembly of microfibrils. Van der Woude syndrome is a condition that affects the development of the face, specifically a cleft lip (see figure 2), cleft palate or both . Carriers of the mutation can also have pits near the centre of the lower lip which may appear to be wet due to the presence of salivary glands. The resulting phenotypes expressed varies significantly among individuals.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
This fact about the conditional, the controversial (for some) law of excluded middle, hinges on reasoning about cause and effect. You might think, for instance, that the fact that it rained is what caused the ground to be wet, if it rained and the ground is wet. But it could well be that it rained after the ground was already wet, or any other possible cause of the observed effect. These other possible causes are called 'hidden variables.
Because Diplocarpon earliana thrives in warm, wet environments, the control of water is important. Without water present, the acervuli are unable to produce conidia and the disease cycle comes to a halt. The leaf tissues should not be wet for more than 12 hours at a time, to reduce susceptibility of the leaf tissue to the production and penetration of conidia. Irrigation can be used to control the amount of water present at all time periods throughout the day.
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Diamonds are naturally lipophilic and hydrophobic, which means the diamonds' surface cannot be wet by water, but can be easily wet and stuck by oil. This property can be utilized to extract diamonds using oil when making synthetic diamonds. However, when diamond surfaces are chemically modified with certain ions, they are expected to become so hydrophilic that they can stabilize multiple layers of water ice at human body temperature. The surface of diamonds is partially oxidized.
Stayton experiences a temperate climate that is usually described as oceanic with mild, damp winters and relatively dry, warm summers, like most of the Pacific Northwest. Summers in Stayton are warm and relatively sunny but can, on occasion, be wet. The warmest month is August with a daytime average of and an average low of . Because of its inland location, Stayton can experience heat waves, in July and August particularly, with air temperatures sometimes rising over .
Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
A contemporary alternative to the traditional, liquid-filled bain-marie is the electric "dry-heat" bain-marie, heated by elements below both pots. The dry-heat form of electric bains-marie often consumes less energy, requires little cleaning, and can be heated more quickly than traditional versions. They can also operate at higher temperatures, and are often much less expensive than their traditional counterparts. Electric bains-marie can also be wet, using either hot water or vapor, or steam, in the heating process.
Toto expects a corresponding improvement in foreign sales within a few years. Another reason is the lack of a power supply near the toilet. While virtually all Japanese washrooms have an electric outlet behind the toilet, many foreign bathrooms lack a nearby outlet. In Australia, New Zealand, Ireland, the UK, and many other countries, high current electrical outlets installed in close proximity to water, or where persons may be wet, are prohibited by codes due to possible health and safety concerns.
Alexander Rossi returned with Manor Marussia. Alexander Rossi became the first American to drive in the United States Grand Prix at the Circuit of the Americas, returning to Manor Marussia after Roberto Merhi had raced for them in Russia. The Sauber team celebrated their 400th Grand Prix in Formula One. The weather was forecast to be wet all weekend, with especially treacherous conditions on Friday afternoon and Saturday, while the race day itself was expected to be slightly less wet.
Cochliobolus lunatus has a widespread distribution, though it is especially prevalent in the tropics and subtropics. Infection is caused by airborne conidia and ascospores, however, sclerotioid C. lunatus can also survive in the soil. The optimal temperature for in vitro growth and infection ranges from 24-30 °C while death results from exposure at 59 °C for 1 minute duration, or 55 °C for 5 minute duration. Successful plant host infection requires the host surface to be wet for 13 hours.
West aspect centered. Mount Larrabee to left As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
The main factors that contribute to the release of the ascospores are moisture and temperature. For the most part, as long as temperatures are above freezing spores can be released, but they are most likely to be released at moderate temperatures of . In the case of moisture, humidity alone is not enough to make the perithecia release the spores, as the perithecia themselves need to be wet. The temperate climates of North America and Europe are most conducive for Eutypella canker development.
Seattle, WA: Mountaineers Books, 2008. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.Beckey, p. 16 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The North Cascades Highway east of Washington Pass has the distinction of being among the top areas in the United States for most avalanche paths per mile of highway.
Table Mountain is situated above the Mt. Baker Ski Area, which recorded the world's greatest snowfall for one season, 1,140 inches (95.0 ft; 29.0 m), which was recorded during the 1998–1999 season. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Both the fallacy of division and the fallacy of composition were addressed by Aristotle in Sophistical Refutations. In the philosophy of the ancient Greek Anaxagoras, as claimed by the Roman atomist Lucretius, it was assumed that the atoms constituting a substance must themselves have the salient observed properties of that substance: so atoms of water would be wet, atoms of iron would be hard, atoms of wool would be soft, etc. This doctrine is called homoeomeria, and it depends on the fallacy of division.
Wooden rolling pin used during the wet felting process In the wet felting process, hot water is applied to layers of animal hairs, while repeated agitation and compression causes the fibers to hook together or weave together into a single piece of fabric. Wrapping the properly arranged fiber in a sturdy, textured material, such as a bamboo mat or burlap, will speed up the felting process. The felted material may be finished by fulling. Only certain types of fiber can be wet felted successfully.
Clifford was born in France in 1788, the illegitimate son of William Cavendish, 5th Duke of Devonshire (and 7th Baron Clifford) (1748–1811), and Lady Elizabeth Foster (1759–1824), daughter of Frederick Hervey, 4th Earl of Bristol. Not long after his birth, his mother brought him to England, to be wet-nursed by Louisa Augusta Marshall, wife of the Rev John Marshall, curate at Clewer, near Windsor, Berkshire. Clifford was educated at Harrow School, 1796–99. His parents married in 1809, their respective spouses having died.
Whereas verification of a theory would prove it, confirmation simply supports it evidentially. But to reason from confirmation to verification is the deductive fallacy called "affirming the consequent": If A, then B; indeed B; therefore A.A physical example makes the illogicality clearer: If it rained, the lawn will be wet; the lawn is wet; therefore it rained. This is illogical since even if B holds, A could be due instead to X or Y or Z, or XYZ combined. A is but one possibility among potentially infinite.
The conservancy covers part of the Shompole group ranch, registered in 1979 and owned by the Loodokilani Maasai with over 2000 registered members. The lodge was closed in September 2011 while the owners discussed its future and that of the conservancy with the local Maasai community. The conservancy has a dry climate, hottest in October and November and most likely to be wet in April and May. Flora are adapted to semi-arid conditions and include umbrella thorn trees and the colorful toothbrush tree.
As with other reservoirs in the North Caspian (Pricaspian) Basin, it is thought that the Karachaganak reservoir was filled over multiple stages, the first of which began during late Paleozoic time with the formation of oil pools. As the basin began to subside, gas was generated and migrated to the traps. The gassiness of the reservoirs is determined by their location in the basin. Northern reservoirs tend to be wet; the southwest part of the basin is more gas prone than are the east and southeast.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. However, Martin's location puts it in the rain shadow of the Olympic Range, resulting in less precipitation than Mount Olympus and the western Olympics receive. The months July through September offer the most favorable weather for viewing and climbing this peak.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
The Sunday Closing (Wales) Act 1881 mandated that all public houses in Wales be closed on Sundays. The Act was extended to Monmouthshire in 1921. Under the terms of the Licensing Act 1961, on the application of 500 local electors, a referendum could be held in each local government area at seven-year intervals on whether that district should be "wet" or "dry" on the Sabbath. Most districts in the border area and the southern industrial area went "wet" in 1961 or 1968, with most others following suit in 1975.
The ráth site, where in ancient times fairs and festivals were held, may date to Celtic times (around 500 BC). In 1556 the Earl of Sussex, Lord Deputy to Elizabeth I, camped with his troops at Dunanney where he met with Irish chieftains and tried unsuccessfully to pacify the Irish people. The name Dunanney has been translated both as 'The Fort of the Assemblies' and 'The Fort of the Watery Place' (built on rock, it tends to be wet and marshy). A second ráth exists to the east of Dunanney.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. This climate supports a small ice remnant on the east side of the pek, and another in the northwest cirque.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Precipitation runoff from the mountain drains into tributaries of the Fraser River and the Nooksack River.
Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
Mount Hermann is situated immediately west of the Mt. Baker Ski Area, which recorded the world's greatest snowfall for one season, 1,140 inches (95.0 ft; 29.0 m), during the 1998–1999 season. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Accuweather released its European forecast on 18 October 2018. They highlighted that conditions in North Western Europe and Western Scandinavia would be wet and unsettled, with frequent windstorms in the United Kingdom, Northern France and Western Norway. Similarly, Southeastern Europe was predicted to have occasional storms, with a swathe of warmer than average temperatures covering most of Portugal and Spain, as well as Italy and extending as far east as South Western Ukraine. Most of Eastern Europe, including parts of Scandinavia were predicted to have 'cold shots', this area extended from eastern Sweden down to Ukraine.
Regarding social issues of his era, Harrington's views on women's suffrage and prohibition caused surprise to many Marylanders. In a state that was widely considered to be "wet", or in favor of legal alcohol, Harrington caused a great deal of upheaval when he announced his support of prohibition, citing concerns for the common welfare. He also surprised his constituents with his support of the proposal to grant voting rights to women, even though he was believed to be against such an initiative. Harrington's term as governor ended on January 14, 1920, and afterwards he returned to his law practice.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above . During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades . As a result, the Cascades experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
On 26 December, Finn-Baltic continued its journey south past the lighthouses of Nordvalen and Kaskinen while maintaining an average speed of 6–7 knots in heavy head seas. In daylight the chief officer noticed that in the forward part of the cargo compartment three or four ore piles had collapsed to half of their original height and the others appeared to be wet. Sea water flowed continuously to the hold and washed ore to the sea through the storm shutters on the sides. However, during the last watch of the day the weather seemed to calm down again.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .
After the two boys were sent to a rural community to be wet nursed, Enrico rejoined his family in Rome when he was two and a half. Although he was baptised a Roman Catholic in accordance with his grandparents' wishes, his family was not particularly religious; Enrico was an agnostic throughout his adult life. As a young boy he shared the same interests as his brother Giulio, building electric motors and playing with electrical and mechanical toys. Giulio died during an operation on a throat abscess in 1915 and Maria died in an airplane crash near Milan in 1959.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
For example, there is a legend that when one is lost in the wild, one only has to cry Mari's name loudly three times to have her appear over one's head to help the person find his or her way. The people of Oñati believed that the weather would be wet when she was in Anboto, and dry when she was in Aloña. In Zeanuri, Biscay, they say that she would stay seven years in Anboto, then the next seven in a cave in Oiz called Supelegor. A similar legend in Olaeta, Biscay substitutes Gorbea for Supelegor.
General-Officer-Commanding Middle East Land Forces, Major- General Philip Tower, feared that it would merely provoke trouble. He was of the view that engaging in a full reoccupation of the Crater, with its risk of casualties, was pointless given that British withdrawal from Aden was imminent and British strategy was moving to the role of neutral peacekeeping. Tower had authorized a probe into the Crater but Mitchell had used this authority to carry out a full military reoccupation. Tower subsequently ordered Mitchell to "throttle back" on the operation. Mitchell stated that he considered Tower's approach to be “wet hen tactics”.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .
Toadmoor Tunnel portal showing elliptical shape of bore Toadmoor Tunnel (originally called Hag Wood Tunnel) was built at Ambergate as part of the North Midland Railway, which opened in 1840.Jewell, R., (1995) Images of Belper & Ambergate, Derby: Breedon Books 128 yards long, it was cut through an unstable hillside on a notoriously difficult line of route. What had initially been expected to be acceptably strong coal-bearing rock turned out to be wet shale. On beginning excavation a landslide occurred, the effects of which can still be seen further up the bank in Thatcher's Wood.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Blue Lake Peak centered, seen from Maple Pass Trail Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
The westerlies explain why coastal North America tends to be wet, especially from Northern Washington to Alaska, during the winter. Differential heating from the Sun between the land which is quite cool and the ocean which is relatively warm causes areas of low pressure to develop over land. This results in moisture-rich air flowing east from the Pacific Ocean, causing frequent rainstorms and wind on the coast. This moisture continues to flow eastward until orographic lift caused by the Coast Ranges, and the Cascade, Sierra Nevada, Columbia, and Rocky Mountains causes a rain shadow effect which limits further penetration of these systems and associated rainfall eastward.
The government has also imposed a 10-year limit (after construction) on claims, even though some building experts believe many cases will only become apparent during coming years, as building rot becomes advanced enough. They also warned that houses in drier parts of New Zealand were now starting to show problems, which had simply developed at a slower pace – and that despite Building Act reforms in 2004, there were still houses being built that leaked badly due to shoddy workmanship. Timber needs a sustained period of wetting to form mould and subsequently rot. In laymens terms, the timber has to be wet longer than it is dry.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Foss Peak (aka Manatee Mountain) As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
Dorado Needle in winter As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
The two things which can directly affect the health of the hoof are diet and exercise. Observers of wild horse populations note that the equine hoof stays in notably better condition when horses are in a herd situation and are free to move around 24 hours a day, as wild horses do, permitting good circulation inside the hoof.The Natural Horse: Lessons From the Wild, Jaime Jackson, Northland Publishing, 1992 It is recommended that horses be allowed to walk at least five miles per day for optimum hoof health. The terrain should be varied, including gravel or hard surfaces and a water feature where the hooves can be wet occasionally.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
The third and final session was still considered to be wet, but a dry racing line had appeared and early times in the session were immediately three seconds quicker than in the second Friday session. Ferrari's dominant streak ended with championship leader Mark Webber fastest before a torrential downpour struck in the second half of the session. Lewis Hamilton was second, with Sebastian Vettel third; Vettel also experienced an unknown mechanical failure and ground to a halt in pit lane. After dominating the Friday practice sessions, Alonso was sixth after an encounter with Jarno Trulli, once again the fastest of the newcomers half a second ahead of Bruno Senna.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
A trail leads from the memorial down into the portage wilderness area. The site commemorates the Chicago Portage, first written about by French explorers Father Marquette and Louis Joliet during their use of the portage and exploration of the area between Lake Michigan and the Mississippi River. The portage crossed what was known as Mud Lake, which could be wet, swampy, frozen, or dry, depending on the season, and which has since been completely obliterated. Mud Lake extended roughly from the historic western end of the South Branch of the Chicago River (near today's Damen Avenue) to the Des Plaines River at the present National Historic Site.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
The ramparts to the south were subject to enfilade fire and were therefore given a greater measure of protection by hiding the guns in a complex range of Haxo casemates. This fort is the only one of the Palmerston Forts to receive such a concentration of Haxo casemates. The fort is surrounded by a ditch that was intended to be wet but problems with obtaining and holding water in this meant that for much of its life the northern portion remained dry. The ditch is ably protected by a grand caponier to the west with smaller demi-caponiers at the north, southwest and south salient angles.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Azurite Peak from east As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, the weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
The Hải Vân Pass crosses over a spur of the Trường Sơn (Annamite) Range that emerges from the west and juts into the South China Sea, forming the Hải Vân Peninsula and the adjoining Son Tra Island. The pass, which once formed the boundary between the kingdoms of Đại Việt and Champa, also forms a boundary between the climates of northern and southern Vietnam, sheltering the city of Da Nang from the "Chinese winds" that blow in from the northwest. During the winter months (November–March), for instance, weather on the north side of the pass might be wet and cold, while the south side might be warm and dry. The pass is renowned for its scenic beauty.
In 1994, now also faced with Cat1 restrictions in the US, Dominicana wet-leased a Boeing 737-300 and a Boeing 757-200 from Mexican low-cost airline TAESA. Further aircraft were wet-leased from Express One International, Atlantic Aviation and Carnival Air Lines. During Christmas of 1994, many Dominicana VFR passengers were stranded at JFK, MIA, and SJU when the airline was unable to provide necessary funding to lessors for heavily-booked Christmas flights (and, overbooked for the B727 the lessors were providing, since an A300 had been expected to be wet-leased). As a consequence of the outrage, in early 1995 the government of the Dominican Republic decided to shut down the airline.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift).Pelton Peak and Pelton Basin from Cascade Pass in summer As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
From about 3,000 years ago until the year 1900, the Des Plaines River and the Chicago River were connected in the ancient stream bed of the Chicago Outlet River by a slough or swampy area known as Mud Lake. This remnant was left behind when the water level of Lake Michigan-Huron dropped as the St. Clair River captured the flow of the Chicago Outlet River. Mud Lake could be wet, dry, marshy, or frozen, depending on the season and the weather, making it a difficult, albeit very valuable, transportation route. It was drained in several stages, starting with the construction of the Illinois and Michigan Canal in 1848, which bisected it.
Finn-Baltic left the port of Raahe with a cargo of 13,398 tons of Malmberget A Fines (MAF) iron ore concentrate bound for the steel factory of Koverhar in Hanko, southern Finland, on 25 December 1990. Baltic had been loaded in Luleå, Sweden, on 21 December and brought to Raahe by the pusher Rautaruukki on the following day to wait for transit to the south. During its stay in Raahe, the barge developed a list of 1–2 degrees to port and the harbour workers noted that the cargo seemed to be wet and some of the ore heaps had collapsed. After the harbour pilot had left the ship the combination turned southwest and headed towards the Kvarken in heavy head seas.
With the stoppage in the second qualifying session, the third session was expanded by half an hour to give teams more time on the circuit. The track continued to be wet but it dried sufficiently enough to allow for an improvement to lap times with 20 minutes left as on- track grip continued to improve. Two stoppages curtailed running in the session: the first was triggered for ten minutes when Christophe Bourret removed the left-front wheel off the No. 77 IMSA Performance Matmut car in an impact with the wall at the first Mulsanne chicane. Jonny Kane in the No. 21 Strakka Racing HPD ARX-03c caused the second red flag after he heavily clouted a barrier and littered debris at the second Mulsanne chicane.
Despite claiming during the off-season that they were a second behind their rivals, McLaren followed Red Bull in claiming the two fastest times in the second session, with Jenson Button a tenth of a second faster than Lewis Hamilton, Alonso and Vettel. Intermittent showers late in the afternoon led to race control declaring the circuit to be wet, but no driver used the wet or intermediate tyres, and a dry line was quickly established. The final half hour was run under race conditions as a simulation of the DRS in order to check that the system was properly implemented. As most of the times during the day had been set with the aid of an unrestricted DRS, no driver recorded a fastest time for the session once the simulation had begun.
According to one tradition, she travelled every seven years between a cave on Mount Anboto and one on another mountain (the stories vary); the weather would be wet when she was in Anboto, dry when she was in Aloña, or Supelegor, or Gorbea. One of her names, Mari Urraca possibly ties her to an historical Navarrese princess of the 11th and 12th century, with other legends giving her a brother or cousin who was a Roman Catholic priest. So far the discussions about whether the name Mari is original and just happened to coincide closely with the Christian name María or if Mari is an early Basque attempt to give a Christian veneer to pagan worship have remained speculative. At any rate, Mari (Andramari) is one of the oldest worshipped Christian icons in Basque territories.
According to Regulation 36 of the Electricity Regulations 1990 a) For a place of public entertainment, protection against earth leakage current must be provided by a residual current device of sensitivity not exceeding 10 mA. b) For a place where the floor is likely to be wet or where the wall or enclosure is of low electrical resistance, protection against earth leakage current must be provided by a residual current device of sensitivity not exceeding 10 mA. c) For an installation where hand-held equipment, apparatus or appliance is likely to be used, protection against earth leakage current must be provided by a residual current device of sensitivity not exceeding 30 mA. d) For an installation other than the installation in (a), (b) and (c), protection against earth leakage current must be provided by a residual current device of sensitivity not exceeding 100 mA.
Since there were no official records kept pertaining to wet nurses or wet nursed children in the United States, historians lack the knowledge of precisely how many infants were wet-nursed, for how long they were wet-nursed, whether they lived at home or else where while they wet-nursed, as well as how many wet-nursed babies lived or died.Golden, Janet, A Social History of Wet Nursing in America: From Breast to Bottle, Cambridge University Press (1996) The only evidence which exists pertaining to wet-nursing in the United States is found in the help wanted ads of newspapers, through complaints about wet nurses in magazines, and through medical journals which acted as employment agencies for wet-nurses. In the Southern United States, it was common practice for enslaved black women to be forced to be wet nurses to their owners' children. In some instances, the enslaved child and the white child would be raised together in their younger years.
The Sabbatarian temperance movement was strong among the Welsh in the Victorian period and the early twentieth century, the sale of alcohol being prohibited on Sundays in Wales by the Sunday Closing Act of 1881 – the first legislation specifically issued for Wales since the Middle Ages. From the early 1960s, local council areas were permitted to hold referendums every seven years to determine whether they should be wet or dry on Sundays: most of the industrialised areas in the east and south went wet immediately, and by the 1980s, Dwyfor in the northwest as the last of the dry regions went wet after a local referendum in 1982; however, in the next referendum it returned to a dry region on Sundays from 1989 to 1996. In early 1996 reconstruction of Gwynedd resulted in Dwyfor district being abolished and Dwyfor area is now covered by an area committee of the Gwynedd Council and there have been no further "Wet - Dry" referendums.
Woman wearing "smoothskin" wetsuit with "beavertail" and twistlock fasteners In 1952, UC Berkeley and subsequent UC San Diego SIO physicist Hugh Bradner, who is considered to be the original inventor and "father of the modern wetsuit," had the insight that a thin layer of trapped water could be tolerated between the suit fabric and the skin, so long as insulation was present in the fabric in the form of trapped bubbles. In this case, the water would quickly reach skin temperature and the air in the fabric would continue to act as the thermal insulation to keep it that way. In the popular mind, the layer of water between skin and suit has been credited with providing the insulation, but Bradner clearly understood that the suit did not need to be wet because it was not the water that provided the insulation but rather the gas in the suit fabric. He initially sent his ideas to Lauriston C. "Larry" Marshall who was involved in a U.S. Navy/National Research Council Panel on Underwater Swimmers.
Plans to wet-lease the remaining aircraft were realised with the December 2016 announcement that 38 Airbus A319/A320 aircraft would be wet- leased to Lufthansa Group's Eurowings (33 aircraft) and Austrian Airlines (five), effective February 2017 for a period of six years. In October 2016, Air Berlin announced plans to close four of its seven airberlin Technik maintenance facilities and lay off 500 of their staff.rbb-online.de – "Air Berlin wants to cancel nearly 500 staff nationwide" (German) 14 October 2016 On 5 December 2016, Air Berlin announced plans to sell its entire 49-percent stake in its Austrian subsidiary Niki to its own minority owner, Etihad Airways.aero.de – "Air Berlin separates Niki and A321-fleet" (German) 5 December 2016 It was also announced that Niki will take over several routes to southern European, north African and Turkish leisure destinations from Air Berlin as part of the new joint-venture.austrianaviation.net – "Finalized: Air Berlin sells Niki to Etihad" (German) 5 December 2016 Also in December 2016, Air Berlin announced the transfer of its entire fleet of 21 A321-200s to Niki and Niki's transfer of all its 5 A319-100s and 13 A320-200s to Air Berlin.
They were unable to sell three of the F27s which had been replaced with F50s the previous year. However, the company was able to downsize easily after 30 pilots resigned to work for SAS Commuter, which expanded its operations in Northern Norway in 1990. It proposed in October that the airline could take over operation of the military Lockheed C-130 Hercules transporters, allowing them to be wet leased on commercial duties when not in regular use, but the idea was squarely rejected by military. Fokker F27-200 Friendships landing at London Heathrow Airport in 1989 Services to Sandefjord were terminated in 1991. This followed an agreement that one Fokker 50 aircraft was to be sold to Widerøe Norsk Air. An important blow came in January 1991, when Busy Bee lost the tender to operate flights for the military, with Busy Be bidding just half a million above Norway Airlines's 100 million kroner. Thus the need for the 737 evaporated from April. This caused the company to reduce its staff from 325 to 200, and reduce its fleet from seventeen to nine aircraft. In September the military announced that it would abolish its leasing operations and instead buy scheduled tickets, terminating the last military charters from 1 April 1992.

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