Eastern wind. east wind east wind name

Education local winds associated with the nature of the underlying surface (orography, type of surface - water or land) and temperature. Breezes are local winds of thermal origin. They are better expressed in cloudless anticyclonic weather and are especially often manifested on the western coasts of the tropics, where the heated continents are washed by the waters of cold currents. We grouped other local winds depending on their properties and origin (temperature or type of landscape over which they form) into three groups: cold, mountain-valley and desert. Separately, the local names of the Baikal winds were given.

local winds

Description of the wind

Cold local winds:

Blizzard

cold piercing wind of storm force in Canada and Alaska (similar to snowstorm in Siberia).

Bora (Greek "boreas" - north wind)

strong, gusty wind blowing mainly in the winter months from the mountain ranges on the coast of the seas. Occurs when a cold wind (high pressure) crosses the ridge and displaces the warm and less dense air (low pressure) on the other side. In winter it causes severe cooling. It occurs in the northwest coast of the Adriatic Sea. Black Sea (near Novorossiysk), on Baikal. Wind speed during bora can reach 60 m/s, its duration is several days, sometimes up to a week.

dry, cold, northerly or northeasterly wind in mountainous regions of France and Switzerland

Borasco, burraska (Spanish "borasco" - small bora)

a strong squall with a thunderstorm over the Mediterranean Sea.

small intense whirlwind in Antarctica.

cold north wind in Spain.

cold wind from Siberia, bringing sharp cold snaps, frosts and snowstorms, in Kazakhstan and the deserts of Central Asia.

sea ​​breeze softening the heat on the northern coast of Africa.

cold northeast wind blowing over the lower part of the Danube lowland.

Levantine

eastern strong, humid wind, accompanied by cloudy weather and rain in the cold half of the year over the Black and Mediterranean Seas.

cold north wind over the coast of China.

Mistral

intrusion of a cold strong and dry wind from the polar regions of Europe along the valley of the Rhone River to the coast of the Gulf of Lion in France from Montpellier to Toulon in the winter-spring period (February, March).

Meltemi

northern summer wind in the Aegean.

cold north wind in Japan, blowing from the polar regions of Asia.

bora-type wind only in the region of Baku (Azerbaijan).

Northser, norter (eng. "norther" - north)

strong cold and dry winter (November - April) northerly wind blowing from Canada to the USA, Mexico, the Gulf of Mexico, up to the northern part of South America. Accompanied by rapid cooling, often with showers, snowfalls, ice.

cold south storm wind in Argentina. Accompanied by rain and thunderstorms. Then the cooling rate reaches 30 °C per day, the atmospheric pressure rises sharply, and the cloudiness dissipates.

strong winter wind in Siberia, lifting snow from the surface, resulting in reduced visibility to 2-5 m.

Mountain-valley winds:

foehns (bornan, breva, talvind, helm, chinook, garmsil) - warm, dry, gusty winds that cross the ridges and blow from the mountains down the slope into the valley last less than a day. Foehn winds have their own local names in different mountain regions.

breeze in the Swiss Alps, blowing from the valley of the river. Drance to the middle part of Lake Geneva.

afternoon valley wind, combined with a breeze on Lake Como (Northern Italy).

Garmsil

strong dry and very hot (up to 43 °C and above) wind on the northern slopes of the Kopetdag and the lower parts of the Western Tien Shan.

pleasant valley wind in Germany.

Chinook (or Chinook)

dry and warm southwest wind on the eastern slopes of the Rocky Mountains of North America, which can cause very large temperature fluctuations, especially in winter. There is a case when in January in less than a day the air temperature increased by 50°: from -31° to + 19°. Therefore, the Chinook is called the "snow eater" or "snow eater".

Desert winds:

samum, sirocco, khamsin, habub - dry, very hot dusty or sandy winds.

dry hot western or southwestern wind in the deserts of the North. Africa and Arabia, swoops in like a whirlwind, closes the Sun and the sky, rages for 15-20 minutes.

dry, hot, strong southerly wind blowing to the Mediterranean countries (France, Italy, the Balkans) from the deserts of North Africa and Arabia; lasts several hours, sometimes days.

sweltering hot and dusty wind blowing over Gibraltar and southeast Spain,

it is a wind with high temperature and low air humidity in the steppes, semi-deserts and deserts, it is formed along the edges of anticyclones and lasts for several days, increasing evaporation, drying up the soil and plants. It prevails in the steppe regions of Russia, Ukraine, Kazakhstan and the Caspian region.

dust or sandstorm in northeast Africa and the Arabian Peninsula.

Khamsin (or "fifty days")

hot gale in Egypt blowing from Arabia for up to 50 consecutive days.

Harmattan

local name for the northeast trade wind blowing from the Sahara to the Gulf of Guinea; brings dust, high temperatures and low humidity.

analogue of khamsin in Central Africa.

Eblis ("dust devil")

a sudden rise of heated air on a calm day in the form of a whirlwind that carries sand and other objects (plants, small animals) to a very high altitude.

Other local winds:

dusty southern or southwestern wind blowing from Afghanistan along the valleys of the Amu Darya, Syr Darya, Vakhsh. It inhibits vegetation, fills the fields with sand and dust, and demolishes the fertile soil layer. In early spring, it is accompanied by showers and cold snaps to frost, destroying cotton seedlings. In winter, it is sometimes accompanied by sleet and leads to frostbite and death of livestock caught on the plains.

strong wind from the Caspian, bringing surge floods to the lower reaches of the Volga.

southeast trade wind in the Pacific Ocean (for example, off the islands of Tonga).

Cordonaso

strong southerly winds along the western coast of Mexico.

the sea breeze blowing from the Pacific Ocean on the coast of Chile is especially strong in the afternoon in the city of Valparaiso, which even suspends port operations. Its antipode - a coastal breeze - is called a terrap.

Probe (sondo)

strong northern or western dry and hot foehn-type wind on the eastern slopes of the Andes (Argentina). It has a depressing effect on people.

prevails in the eastern Mediterranean, warm, brings rain and storms (lighter in the western Mediterranean)

fair wind on rivers and lakes.

Tornado (Spanish: Tornado)

a very strong atmospheric vortex over land in North America, characterized by high frequency, is formed as a result of the collision of cold masses from the Arctic and warm masses from the Caribbean.

One of the most dangerous winds in Chukotka. The strongest constant wind in the world, its usual speed is 40 m/s, gusts up to 80 m/s.

Winds of Baikal:

Verkhovik, or hangar

north wind overpowering other winds.

Barguzin

northeast storm wind blowing in the central part of the lake from the Barguzin valley across and along Baikal

local southwest storm wind bringing overcast weather.

Harahaiha

autumn-winter northwest wind.

southeast storm wind blowing from the valley of the river. Goloustnoy.

cold strong chilling winter wind blowing along the river valley. Sarma.

_______________

A source of information: Romashova T.V. Geography in figures and facts: Educational manual / - Tomsk: 2008.

Eastern wind

East wind (Heb. khadim), dry, burning and harsh wind (Job 27:21; 38:24; Isaiah 27:8) , which blows from the sandy deserts of Arabia (Hos 13:15; Job 1:19; Jer 4:11; 13:24) . In Palestine, the weather, as determined by W.V., is generally from April to mid-June and from mid-September to October. V.V. always lasts several days, the spring vegetation dries up during this time (Ezek 17:10; 19:12; Jonah 4:8; Ps 102:15,16; cf. Isaiah 40:7,8) . If V.V. starts to blow in early spring, it can cause a mean. crop damage (see Gen 41:6). In Egypt, this wind often brought clouds of locusts (Ex 10:13). Under the "south wind" (Greek notos) in Luke 12:55 it also refers to the hot, dry wind of the deserts.


Brockhaus Bible Encyclopedia. F. Rinecker, G. Mayer. 1994 .

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Answer from Igor[guru]
The trade wind is a wind that blows between the tropics all year round, in the Northern Hemisphere from the northeast, in the Southern Hemisphere from the southeast, separated from each other by a calm strip. On the oceans, the trade winds blow with the greatest regularity; on the continents and on the seas adjacent to the latter, their direction is partly modified under the influence of local conditions. In the Indian Ocean, due to the configuration of the coastal continent, the trade winds completely change their character and turn into monsoons.

Origin of the trade winds
Due to the action of the sun's rays in the equatorial strip, the lower layers of the atmosphere, heating up more, rise up and tend towards the poles, while new colder air currents come from below from the north and from the south; due to the daily rotation of the Earth according to the Coriolis force, these air currents take in the Northern Hemisphere the direction towards the northeast (northeast trade wind), and in the Southern Hemisphere - the direction to the southeast (southeast trade wind). The closer any point on the globe lies to the pole, the smaller the circle it describes per day, and therefore, the less speed it acquires; thus, air masses flowing from higher latitudes, having a lower speed than the points of the earth's surface on the equatorial strip, rotating from west to east, must lag behind them and, therefore, give a flow from east to west. At low latitudes, close to the equator, the difference in velocities for one degree is very small, since the meridian circles become almost mutually parallel, and therefore in the band between 10 ° N. sh. and 10°S sh. the inflowing layers of air, in contact with the earth's surface, acquire the speed of the points of the latter; as a result, near the equator, the northeast trade wind again takes an almost northerly direction, and the southeast trade wind almost south and, meeting each other, give a strip of calm. In the trade winds between 30 ° N. sh. and 30°S sh. two trade winds blow in each hemisphere: in the Northern Hemisphere, northeast at the bottom, southwest at the top, southeast at the bottom, and northwest at the top. The upper course is called the anti-trade wind, counter-trade wind, or upper trade wind. For 30 ° north and south. sh. the upper, coming from the equator, layers of air descend to the surface of the earth and the regularity of the equatorial and polar currents ceases. From the polar boundary of the trade wind (30 °), part of the air mass returns to the equator as a lower trade wind, and the other part flows to higher latitudes and appears in the Northern Hemisphere as a southwest or west wind, and in the South - as a northwest or west wind .
Historical perspective
lower trade winds between the tropics; on the Atlantic and Pacific oceans, were known to the sailors of antiquity. The satellites of Columbus were greatly alarmed by these winds, which carried them non-stop to the west. The correct explanation of the origin of the trade wind was first given by Gadley (1735). The windless strip moves north or south, depending on the state of the sun at the equator; in the same way, the boundaries of the trade wind region change both in the north and in the south at different times of the year. In the Atlantic Ocean, the northeast trade wind blows in winter and spring between 5° and 27°N. sh. , and in summer and autumn between 10° and 30° N. sh. . The southeast trade wind reaches 2°N in winter and spring. sh. , and in summer and autumn 3 ° N. sh. , thus passing through the equator and gradually turning into a southerly and southwesterly wind.
Special maritime terminology.
East wind - stop.
Northeast wind - northeast.
Southeast wind - southeast



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