Climate in United States of America. Temperatures in different parts of United States of America
United States of America located in the central part of the North American continent, occupying a immense arrondissement between 25 th and 57 th parallels of north latitude. To the east, washed Atlantic, in the south - the Gulf of Mexico Caribbean Flood in the west and south-west - the Pacific Lots, the northern and north-west beach of Alaska - the Arctic Ocean.
U.S. borders with Canada in the north (the add up to magnitude of 8893 km limits, including 2,477 km in Alaska), with Mexico in the south (3141 km), with Russia in the north-west (quantity frame to the Bering Limiting and the Arctic shelf, the detach between the islands of Lesser and Obese Diomede, affinity to the Joint States and Russia, severally, is solely 4 km) and Cuba in the south-east (the border as the swell, the Straits of Florida, and on arrive, in the U.S. naval post at Guantanamo Bay, located directly in Cuba).
The Hawaiian Islands are located in the dominant Pacific The drink flood, a distance of almost 4000 km from the mainland. Varied cay territories, and in whole form or another owned by the U.S., scattered across the waters of the Pacific and Atlantic oceans.
Subservient to the supervision of the United States is also a number of isle territories with other civil repute (in each case, it installs a classify pact, backed before the finding of the federal authorities). These contain the ait territory of American Samoa, Guam, Northern Mariana Islands, Marshall Islands, Federated States of Micronesia, Puerto Rico, U.S. Virgin Islands, Baker, Howland Atoll and Jarvis Cay, Johnston Atoll, Midway Holm, Navassa Island, Palmyra, Wake, Kingman Reef and some other territory.
The total parade of the country is about 9,360,000 l- meters. km (9,820,000 honourable meters. kms - with the islands and the Assign Territories).
Aura and live through
Weather USA is a abundant variety of climatic conditions. At the gist of the country induce identified two main climatic department - East and West. The bounds between them coincides with isohyet 500 mm and should be roughly along the meridian 100 ° W
Eastern district as a whole is characterized by clammy weather with an usually annual rainfall of 500 mm along the meridian 100 ° W to more than 1500 mm in the south-east. The cardinal source of rain - genial moist song coming from the Inlet of Mexico, and - to a much lesser extent - from the Atlantic Ocean. Temperatures in this region are more influenced around latitude than the height of the integument, and measure uniformly increased from north to south. As a consequence, short summers in the north and intense in the south long and acrid, and winters in the north has a crave and chill, in the south is knee-pants, and dialect right warm.
Weather tomorrow New York. Much of the eastern region source to everyday live through changes, mainly because the emanate of animated breath from the south much interrupted the masses of numbing manner infiltrating from the north. Specifically changeable sickly in Late England, where wordy rainy seasons quickly replaced cloudless dry.
In the Western Ambit mountainous terrain has a excessive change on the circulation of the atmosphere. When vlagonesuschie aerate masses unfixed from the Pacific Ocean to the east, rising more than the considerable mountains, where precipitation. Commensurate with explain, the windward western slopes of the mountains is much better supplied with moisture, than the jumbo arid range located on the leeward side of the shower track of mountains. Although in comprehensive the Western Province is inborn in the arid climate, mean annual sleet ranges from less than 120 mm in the Sonora desert to more than 2500 mm in some areas the Shore Ranges.
Temperatures in the western ambit depends on latitude and altitude, and in coastal areas studied past moderating the contact of the ocean. The highest of the mountains are constantly in the winter, whereas in the most southern empty most of the year dominated through unpredictable intensify weather. Unstable Mountains to watch over them from the infringement of cold air masses from the north.
Climatic regions. On the mainland, the U.S. gives 11 climatic regions, including four in the Eastern climatic dominion and seven - in the West.
Sticky continental ambience with momentary summers covers the northern states from North Dakota to Maine. Summer is stubby and there is a amorous, daytime maximum temperatures (27-38 ° C) were observed in fine climate ailing, much slash - in the cloud. The frost-free spell, underfunded - from less than 120 days in North Dakota to about 180 days in the Point Point Cod in Massachusetts. The winters are wish and apathetic, in many cases with daytime supreme temperatures lower 0 ° C.
Average weather Chicago. Standard in the main annual downpour ranges from 500 mm in the west to over 1000 mm on the strand of New England. At least half of the overall snowfall falls in summer, and they commonly bear vociferous character. Winter downpour normally falls as snow. Greatest capacity of snow defend in the mountains of Rejuvenated England and firstly in the valley r.Sv. Lawrence.
Sticky continental ambience with prolonged summer includes most of the Midwest and is characterized by way of long blistering and wet summer. Sweltering summer days, the maximum temperatures exceed 32 ° C, the nights are warm. The greater part of the partition frost-free age lasts from 150 to 200 days, which creates favorable conditions instead of growing corn and other crops. Winters are emotionless, but there are periods of mild suffer, often with fog.
Ordinary annual snow ranges from 500 mm in the west to over 1000 mm on the slide of New England. At least half of the utter downpour falls in summer, and they in many cases have torrential character. Winter sleet as per usual falls as snow. Peak capacity of snow enclose in the mountains of Unfamiliar England and especially in the valley r.Sv. Lawrence.
Soggy continental feel with lengthy summer includes most of the Midwest and is characterized through protracted hot and humid summer. Piping hot summer days, the maximum temperatures exceed 32 ° C, the nights are warm. The greater part of the neighbourhood frost-free space lasts from 150 to 200 days, which creates favorable conditions pro growing corn and other crops. Winters are cold, but there are periods of equable indisposed, oft with fog.
Common annual hail ranges from 500 mm in the west to wellnigh 1300 mm in the east, with their most falls in the form of summer showers. Although snowfalls are annual, winter snowfall primarily rain.
Humid subtropical aura occupies all but the unexceptional country to the south of the wet continental climate. Summer is long and commercial: scalding and steamy time (most temperature 32-38 ° C); only one nights cooler, but usually not less wet. Frost-free aeon lasts 200 days in the north to more than 300 days on the Fiord Coast. In some years there is no winter frost. Winters everywhere in the sphere are uncivil and mellow, the superlative daytime temperatures of 10 to 21 ° C.
In most of the arrondissement falls year on customarily 1000-1500 mm of rain in the west - only 500 mm. The dissemination of downpour on seasonal uniform. They decrease mainly in the fashion of rain. In late summer and autumn coastal areas sometimes suffer from tropical storms, which differ tremendous opposing force.
Sultry and sizzling tropical feeling is the most southern say of Florida. This is the one precinct really tropical atmosphere on the mainland In harmony States. This year round there are no keen-minded seasonal and routine fluctuations in temperature. Afternoon apogee temperatures are typically 21-32 ° C, and at gloaming just 6 ° C below. Fair-minded as in the subtropical climate, here dear applicable humidity and constantly stuffy. Norm annual showers exceeds 1500 mm, with most of their accounts object of the epoch from May to October.
Part temperate maritime aura is confined to the Pacific Northwest within the Pacific regional mining district, north of San Francisco Bay. Influenced by the prevailing westerly winds blowing from the Pacific The depths, summer here is cooler and winters warmer than other places the U.S., located on the for all that latitudes. Summer is on the whole lively, limit common temperature 21-26 ° C and least night - 10-15 ° C. Winters are mild, with temperatures most often vulnerable 0 ° C, the crest daytime temperature rises to 4-15 ° C. The frost-free epoch lasts from 200 up to 300 days, and glacial are usually alone at night.
Weather five day forecast. Average annual rain ranges from 750 to 3600 mm and more, with the most sultry western slopes of the Coast Ranges. Although the rains fall year about, most of them in the character of continuous sunshower or drizzle in the lead-gray sky falls on winter. Clouds typical winter weather, and in solution with persistent stifle bewilder and low-hanging cloud, the weather reminds protracted drizzle with dull in Western Europe. Every year, winter is a some days with snowfalls, but the snow kept sole on the tops of the mountains. As probably as on the Pacific Ocean. August and September - the warmest months (+24-30 ° C), January and February - the most phlegmatic (about +12 ° C) and the wettest, but at any chance, the gobs breezes soothe the ill in the government of greater comfort. But, urban smog in conjunction with the summer fury makes the outshine of summer is not the most superbly point to stop the metropolis, while adjoining the northern and southern resort areas in the unmodified duration, take first-rate out of sorts conditions.
The clime of Alaska more bleak, since 30% of its vicinage is located within the Arctic Circle. In northern and pre-eminent areas, with their sub-Arctic weather, the thermometer in winter over again fall-off to -45-50 ° C, in summer the air was tempestuous to +16-20 ° C (in the northern regions - +2-6 ° C) with remarkably down rainfall (about 250 mm annually). In southern and key parts of the clime is temperate maritime, mean summer temperature is on all sides +18 ° C, but often the air is frenzied to +30 ° C) in winter - from -6 ° C to +4 ° C, drizzle is falling from 400 to 600 mm per year.