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70 Sentences With "be very hot"

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

Going in, everyone knew this year's session could be very hot.
Jason Momoa proves that long hair done right can be very hot.
It can be very hot in the summer and bitter in winter.
Then carefully transfer it into the pot (the Dutch oven will be very hot).
"When William and Kate arrive they can expect it to be very hot," he continues.
It's going to be very hot and that will make my serve a little faster.
When the events are happening, we expect many people to come and the weather will be very hot.
Oh, and while we're on the topic, did we mention that his father also happens to be very hot?
If you're not using a food processor, mix the dough with a spoon or chopsticks because the dough will be very hot. 2.
Sex dreams can be very hot or very awkward, but for the most part they're nothing more than entertaining because they live in your subconscious.
Investing in real estate above the Arctic Circle might be a real long-term winner, but at our latitude, where it will be very hot, it would be a loser.
Snap: yes, we want your IPO support, and no, you can't see our booksHow far will banks go to be part of an initial public offering that probably will be very hot?
A pair that you've hedged a lot of bets on and think that is going to be very hot, eight months later doesn't end up being so hot because the kids don't get into it.
Additionally, transportation time for all chickens and turkeys cannot exceed four hours, since they are not given food or water during transport and trucks are not climate-controlled, which can mean they can be very hot or cold.
"The coverage of the Knicks in this city can be very hot-takey, and we wanted to produce content that was nuanced but also honest," said Jonathan Macri, a special-education teacher in Brooklyn and the site's lead writer and podcast host.
Water extracted from the bore-wells has been found to be very hot.
The day was expected to be very hot, and the officials wanted to avoid the heat of the late morning.
While summers can be very hot (exceeding 35C) the winters are mild in Hajira, with snowfall very rare due to the low altitude.
An ostrich can keep its body temperature relatively constant, even though the environment can be very hot during the day and cold at night.
Despite the modest elevation, the city has a continental climate with cold winters (lowest recorded temperature is in January 1985). Summers can be very hot (highest recorded temperature of in July 1983).
"I know that the weather will be very hot") and propositional attitude (e.g. "I think that we should stay at home today"), plus oblique and indirect object relativisation. # Utterance (e.g. "He said that he was tired").
The Bureau of Meteorology classify this climatic zone as the Hot Dry Zone (with cooler winters). Places in this zone can be very hot in the summer months while in the winter, nights can be very cold.
Winters are cold with temperatures, sometimes lower than 3°C. The summers can be very hot, with temperatures over 37°C. Yuncler is a village where there is not a lot of rain data, but sometimes there are rainstorms.
Temperatures can thus be very hot in summer and the downpours brutal, the Tricastin valley being located as it is between the Cévennes Piedmont (in the Gard and Ardèche departments) and the town of Nyons in the Baronnies (Drôme and Vaucluse).
The village is on the Karakoram Highway, the main road for expeditions to Karakoram. The surrounding mountains create sharp variations in weather, and the temperatures can sometimes be very hot in the summer during the day, but are always cold at night.
These natural resources make Huating a rich land where everything grows, from staple food such as rice, wheat, oats to specialty plants and vegetables very local. The weather is mild and wet, with a lot of rain in summer which tends to be very hot and humid.
Hiking and recreation at Strawberry Crater is open year round. Winters near the crater average to around 50 degrees, while summers tend to be very hot and dry. There are very few natural water sources near the hiking trail, so travelers are advised to bring a sufficient amount of water.
Juna Savar is situated on southern Saurashtra plateau. It has a hilly terrain and the ground water table is very low. The water contains high level of TDS counts along with excess level of sodium and phosphet. The water extracted from the bore-wells is found to be very hot.
Although in the southern range of the Chihuahuan desert, due to its altitude, Real can be very cool at night. Although days, particularly in summer, can be very hot, it is advised to always bring a jacket, even in summer. Real de Catorce was named a "Pueblo Mágico" in 2001.
Jabal is situated on the southern Saurashtra plateau, and has a hilly terrain. The ground water table is very low. The water contains high level of TDS counts along with excess level of sodium and phosphate. The water extracted from the bore-wells is found to be very hot and salty.
Wadegaon lies on the Tropic of Cancer and becomes very hot during the summer, especially in May. Although it can be very hot in the day, it is cool at night. The annual rainfall averages 850 mm. Most of the rainfall occurs in the monsoon season between June and September, but some rain does fall during January and February.
Sinks, windows and bathrooms are often missing. These buildings can be very hot or very cold depending on the year and often leak when it rains. In the Colonial Forestal kindergarten, 85 children receive their education in a construction of this type. It was founded in the 1990s, by the Instituto Estatal de Educacion Publica de Oaxaca.
El Mirage Lakebed experiences a desert climate, with cool winters and hot summers. Due to the lakebed's aridity and high elevation, the diurnal temperature variation is substantial. Though summer days can be very hot, summer nighttime temperatures are cool. The lakebed receives an occasional dusting of snow in the winter months, however, snowfall usually melts within 24 hours.
Köppen climate types in New South Wales The major part of New South Wales, west of the Great Dividing Range, has an arid to semi arid climate. Rainfall averages from a year throughout most of this region. Summer temperatures can be very hot, while winter nights can be quite cold in this region. Rainfall varies throughout the state.
Fluorine has only one stable isotope (F-19), and does not easily become radioactive under neutron bombardment. Compared to chlorine and other halides, fluorine also absorbs fewer neutrons and slows ("moderates") neutrons better. Low-valence fluorides boil at high temperatures, though many pentafluorides and hexafluorides boil at low temperatures. They must be very hot before they break down into their constituent elements.
Winter (Dec-Feb) temperatures in Mountain House range from 30s to 60s. Springs (Mar-May) in Mountain House are mild with temperatures in the range of 40s to 80s. Summers (Jun-Aug) can be very hot with temperatures in 80s to 100s. Fall (Sep-Nov) temperatures start hot in the 80s to 100s but cool down significantly by November 40s to 70s.
Like all the rivers in Vosges it is subject to an oceanic regime which is characterized by high winter waters and low summer waters, contrary to the Rhine. The last catastrophic flood occurred in May 1983. The climate is of semi-continental type with about 600 mm of rain per year. Temperature differences are particularly marked: summers can be very hot and the winters harsh.
As a crucible will be very hot when heating it in a furnace or a Bunsen burner, one cannot hold the crucible directly. Therefore, crucible tongs come to play a key role when burning, or doing anything with hot objects. The major types of metals used to produce the tongs are stainless steel, brass, and nickel. Moreover, some of them also have a special characteristic.
The Australian Bureau of Meteorology classify this area as the Hot Dry Zone (with cooler winters). Places in this zone can be very hot in the summer months while in the winter, nights can be very cold. Because of the hot and arid climate there are no towns within Conoble although a now disused Railway platform was operated from 1919 until 1986.Conoble Railway Station.
The climate experienced is humid subtropical (Köppen: Cfa) of the type found in the deep south, especially far from the coast. Autumn, winter and spring are mild, with occasional winter nights below freezing but rarely extended cold and rigorous. Florence's summers can be very hot and humid. The city, like others in the Southeast, is prone to inversions, which trap ozone and other pollutants over the area.
If you leave the trail and start scaling the rocks you will find out quickly that 1.5-billion-year-old mudstone is very brittle and not a very reliable handhold. Climb around with caution. In the daytime it can be very hot, but nights are very cold, so pack accordingly. Though the Missions aren't huge, it is always a good idea to bring a map.
It is difficult for them to adapt to the noisy city life. They are depressed living in concrete housing, which can be very hot during the day and stays hot all night. They were more comfortable living in the peaceful and cool environment of the old village, where there are full of green trees that protects them from sunlight. Besides, they felt freer there.
She beats it up with a cast iron skillet, but the underwear beats her back and dives into the water. Then along comes Porky with a box of hot tamales (which, as we will see later, prove to be very hot). He's making his rounds and takes a brief break. A nearby chicken eyes the box of tamales, opens it up and swallows a tamale whole.
There are many big windows, so in summer the rooms can be very hot. Everything is very nice and new. Three elevators provide access to the three floors. The 36 classrooms are in four blocks: A, B, C and D. In block A there is the school hall. During the breaks you can buy things to eat and at lunch time you can buy food in the Cafeteria called “Coffito”.
Haldia has a tropical savanna climate (Köppen climate classification Aw), with winter temperatures ranging from a low of around degrees Celsius to a high of . Summers can be very hot and humid. Usual summer temperatures in May, the hottest month range from a low of degrees to highs around degrees. Although summers are hot and humid, Kalbaishakhis provide a relief to the people, albeit killing some in the process.
Unlike an incandescent bulb, the filament is not the source of light in deuterium lamps. Instead an arc is created from the filament to the anode, a similar process to arc lamps. Because the filament must be very hot before it can operate, it is heated for approximately 20 seconds before use. Because the discharge process produces its own heat, the heater is turned down after discharge begins.
Vientiane features a tropical savanna climate (Köppen Aw) with a distinct wet season and a dry season. Vientiane's dry season spans from November through March. April marks the onset of the wet season which in Vientiane lasts about seven months. Vientiane tends to be very hot and humid throughout the course of the year, though temperatures in the city tend to be somewhat cooler during the dry season than the wet season.
HD 136118 b is a brown dwarf located approximately 171 light-years away in the constellation of Serpens Cauda. This object had a minimum mass of 11.9 times that of Jupiter. Due to its high mass the planet is likely to be very hot and possibly glowing faintly. The lower limit on its mass is only slightly less than the deuterium burning threshold that some astronomers use to distinguish between planets and brown dwarfs.
It is an extensive semi flat area bordered by the Sierra Madre de Chiapas, the Central Highlands and the Northern Mountains. Within the depression there are a number of distinct valleys. The climate here can be very hot and humid in the summer, especially due to the large volume of rain received in July and August. The original vegetation was lowland deciduous forest with some rainforest of middle altitudes and some oaks above above sea level.
They are predominantly of rainfall origin, mostly not from Hungary, but from the surrounding higher-lying parts of the Carpathian Basin. This water, when brought to the surface from great depths, is rich in various mineral solutions and may be very hot. Deep boring for stratum water has been carried out throughout the country. There are about twenty-eight thousand artesian wells in the Great Plain alone, out of a total of thirty-five thousand for the whole country.
It was well known to organizers that Phoenix can be very hot during summer, but nonetheless, Phoenix inherited the Detroit race's scheduled slot of June 4, 1989.New site for Grand Prix race, Observer Reporter Washington, associated press June 4, 1989 The city had only 4 months to finish the 2.36 mile long circuit. This required fencing off and repaving the road surface, as well as building grandstands, garages for the pit crew, and other infrastructure.
Ballowal features a semiarid climate under the Köppen climate classification, with three defined seasons; summer, monsoon and winter. Summers, which range from April through June in the village, tends to be very hot and very dry with average highs in May and June hovering around 40 degrees Celsius. The monsoon season which runs from July through September, sees a slight decrease in average temperatures but an increase in humidity. The bulk of the village’s annual precipitation is received during the monsoon season.
Summers can be very hot, due to its inland location, usually averaging 30ºC from December to March, but sometimes peaking near 40ºC during the hottest of days. This is due to the Du Toitskloof and Riviersonderend Mountains blocking cooling oceanic breezes from reaching the valley. During winter however, the valley is often colder than other seaward regions, like the Overberg. Snow is a regular occurrence on the surrounding mountains; snow does not fall on the valley floor, although light frost does occasionally occur.
This allowed Leo to morph into the Red Galaxy Ranger and serve as the team leader. Fittingly for his element (Fire), Leo has shown to be very hot- headed and impulsive at times, although this changes as the series progresses. Throughout the series, Leo's arsenal included the Magna Talon Transdagger, Red Astro Cycle, Armor Keys (which he used to become the Red Armored Ranger), Red Capsular Cycle (which he gained through understanding his Galactabeast), and the Lights of Orion. He also piloted the Lion Galactabeast/Lion Galactazord.
Accommodation stops are usually 6-8 hours apart, and include guest houses, country hotels, game lodges, nature reserve cottages and farm stays. Most of these stops are fully serviced, allowing riders to travel light. Coolest times for the trail are the autumn months of March to May, and in the spring from September to early October. The summer months from November to February may be very hot, while winter months from June to August may be very cold, with possible snowfalls at high points along the route.
A prominent feature of the climate in this region is the sirocco, a dusty, choking south wind blowing off the desert, sometimes at gale force. This wind also occasionally reaches into the coastal Tell. In Algeria only a relatively small corner of the Sahara lies across the Tropic of Cancer in the torrid zone, but even in winter, midday desert temperatures can be very hot. After sunset, however, the clear, dry air permits rapid loss of heat, and the nights are cool to chilly.
The wettest calendar year since 1894 has been 1957 with and the driest 1939 with , whilst the wettest single month has been May 1981 with During the summer, days can be very hot, with maxima of on 28.5 afternoons and over on 1.1, although mornings very rarely stay above . The record hottest temperature is on July 21, 1931 and the hottest morning on July 31 of 1936. The fall season is usually short and variable, with snow occasionally falling in September, but at other times hot weather can extend into October or even November.
The Bureau of Meteorology classify the Riverina in the Hot Dry Zone (with cooler winters) climatic zone. Places in this zone can be very hot in the summer months while in the winter, nights can be considerably cold with cool to mild days. Mean daily maximum temperatures in the Riverina range from in January and in July in Wagga Wagga to in January and in July in Hillston. Rainfall levels in the Riverina are generally low with the median annual rainfall over most of the region between , rising to between on the eastern fringe.
Summerlin has a hot desert climate typical of the Mojave Desert in which it lies (Köppen climate classification: BWh). Due to its relatively higher elevation, Summerlin is often a few degrees cooler than Downtown Las Vegas and the Las Vegas Strip and may receive slightly more precipitation. Clear skies and sunshine are abundant year-around, with 310 days of sunshine per year and low humidity in every season. Summers tend to be very hot and very dry, with daily highs often exceeding ; temperatures as high as 118 degrees have been observed.
Bledug Kuwu mud volcano, Central Java, Indonesia. Grobogan is a flat valley lying between two mountains, Pegunungan Kendeng to the south and Pegunungan Kapur Utara to the north. Although the town is known to be very hot during the dry season, Grobogan is one of the main rice producers in Central Java, which mainly supported by several man-made dams, such as Bendungan Klambu, Bendungan Sedadi and Bendungan Kedung Ombo. The construction of Bendungan Kedung Ombo was a source of national debate due to the social cost of this gigantesque project supported be the World Bank.
Paso Robles often receives less than 10 inches (250 mm) of rain per year and typically, no rain falls from May through September. Summers in Paso Robles tend to be very hot, with daily temperatures frequently exceeding from late June to as late as mid September, and occasionally exceeding . Paso Robles' summers feature an unusually large daytime-nighttime temperature swing, where there may be a profound temperature difference, as much as 50 °F (28 °C), between the daytime highs and the overnight lows. Winters are often very cool and moist, with daytime temperatures reaching into the low 50s°F (10 °C).
Relief Map In this wilderness area visitors are advised to carry sufficient fuel, food, water and medical supplies since there are no services and cellphone coverage is sparse. At an elevation of , days can be very hot and nights quite cold. The climate is dry, with most rain falling in winter and annual totals averaging about . Walking in the Carrizo Plain area can be dangerous due to low humidity, temperature extremes and rattlesnakes; and is also difficult due to tall grass hiding a very irregular ground surface created by the many burrowing mammals including an endangered species of kangaroo rat.
One of the distinguishing physical properties helpful for identifying euchlorine in hand sample is its streak, which is a pistachio-green color. If trying to find euchlorine in the field, wear protective clothing as the volcanic fumaroles around which it occurs can be very hot (approximately 300 to 650°C, 580 to 1200°F) and can cause severe steam burns if not adequately protected.Balassone, G., Petti, C., Mondillo, N., Panikorovskii, T.L., de Gennaro, R., Cappelletti, P., Altomare, A., Corriero, N., Cangiano, M., and D’Orazio, L. (2019) “Copper Minerals at Vesuvius Volcano (Southern Italy): A Mineralogical Review“.
The course spans the entire Gaza Strip, from Beit Hanoun near the border with Israel in the northeast to Rafah, near the Egyptian border in the south. From Beit Hanoun the course runs west toward the Mediterranean coast, and then follows the coastal road southwest, parallel to the coast, before turning inland to Rafah. The route passes battered towns, refugee camps, the fishing harbor, the ruins of Yasser Arafat's former presidential compound, and the shells of other buildings hit in Israeli air strikes. The course is mostly flat but conditions in May tend to be very hot.
Leavenworth has a continental Mediterranean climate (Köppen Dsb) with summers characterized by hot, sunny days and chilly nights, and cold, snowy winters. During the summer, the weather is typically anticyclonic due to the presence of the North Pacific anticyclone, with resultant clear skies and large diurnal temperature ranges. Rainfall is limited by the Cascade rain shadow as well as by the anticyclone, and all months from May to October have recorded zero precipitation on occasions, including 114 consecutive days without precipitation from June to October 2003. When a continental flow enters the Columbia Basin, the temperature can be very hot during the day, with the hottest temperature being during the heatwave of July 1941.
Al-Bukayriyah is part of the climatic conditions in which we find in the Najd region, which is the desert climate that is known to be very hot in summer and very cold in winter. What distinguishes Al-Bukayriyah is that the climate during the summer is less hot compared to the climate of Najd, and this is due to the effect of the farms and orchards surrounding Al-Bukayriyah, as it contributes to tempering the temperatures in the summer, especially since many farms are located in the heart of Al-Bukayriyah and its near ends, which softens the temperatures due to moisture as The density of vegetation causes moderate temperatures in summer. Also, rain falls on Al Bukayriyah in winter due to the western winds.
Vineyards of Chateau Indage in Pune While a large portion of the Indian subcontinent is not ideal for viticulture, the large diversity of climate and geology does cover some areas with suitable terroir for winemaking to thrive. The summer growing season in India tends to be very hot and prone to monsoons. Many of India's wine regions also fall within the tropical climate band. Vineyards are then planted at higher altitudes along slopes and hillsides to benefit from cooler air and some protection from wind. The altitude of India's vineyards typically range from around 660 ft (200 m) in Karnataka, 984 ft (300 m) in Maharashtra, 2,600 ft (800 m) along the slopes of the Sahyadri to 3,300 ft (1000 m) in Kashmir.
Located in the western part of the country among the foothills of the Andes, the major wine regions of Argentina have a semi-arid desert-like climate owing to low annual precipitation and rely on irrigation from the melting snow caps of the mountains for viticulture. The major wine regions of Argentina are located in the western part of the country among the foothills of the Andes Mountains between the Tropic of Capricorn to the north and the 40th parallel south. Most of the regions have a semi-arid desert-like climate with annual rainfall rarely exceeding more than a year. In the warmest regions (such as Catamarca, La Rioja, San Juan and the eastern outreaches of Mendoza), summer temperatures during the growing season can be very hot during the day with temperatures upwards of .
Typically, a heat spike is characterized by the formation of a transient underdense region in the center of the cascade, and an overdense region around it. After the cascade, the overdense region becomes interstitial defects, and the underdense region typically becomes a region of vacancies. If the kinetic energy of the atoms in the region of dense collisions is recalculated into temperature (using the basic equation E = 3/2·N·kBT), one finds that the kinetic energy in units of temperature is initially of the order of 10,000 K. Because of this, the region can be considered to be very hot, and is therefore called a heat spike or thermal spike (the two terms are usually considered to be equivalent). The heat spike cools down to the ambient temperature in 1–100 ps, so the "temperature" here does not correspond to thermodynamic equilibrium temperature.
In high-energy particle colliders, matter creation events have yielded a wide variety of exotic heavy particles precipitating out of colliding photon jets (see two-photon physics). Currently, two-photon physics studies creation of various fermion pairs both theoretically and experimentally (using particle accelerators, air showers, radioactive isotopes, etc.). It is possible to create all fundamental particles in the standard model, including quarks, leptons and bosons using photons of varying energies above some minimum threshold, whether directly (by pair production), or by decay of the intermediate particle (such as a W boson decaying to form an electron and an electron-antineutrino). As shown above, to produce ordinary baryonic matter out of a photon gas, this gas must not only have a very high photon density, but also be very hot – the energy (temperature) of photons must obviously exceed the rest mass energy of the given matter particle pair.

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