what wind belt is closest to the equator

May 04,  · The Earth rotates beneath this moving air, causing it to turn to the west and creating the easterly trade winds. Because these trade winds converge near the equator, the tropical rain belt is known to meteorologists as the Inter-tropical Convergence Zone. Click buttons to play/advance. Monthly average global rain rates. Reveals how differences in solar radiation create the global wind belts, and how global winds influence climate. %.

The Sun heats the ocean, evaporating tremendous amounts of water. The sun-warmed ocean heats the overlying air, which rises like a hot air balloon. As air rises, it cools, and water vapor condenses into how to cite ethics code apa. The rising air near the equator is replaced by air from north and south of the equator.

The Earth rotates beneath this moving air, causing it to turn to the west and creating the easterly trade winds. Because these trade winds converge near the equator, the tropical rain belt is known to meteorologists as the Inter-tropical Convergence Zone. Monthly average global rain rates. The sequence begins in March, when summer is drawing to a close in the Southern Hemisphere. The highest rain rates on the what happened at the first battle of bull run blue occur south of the equator, and places like Madagascar, northern Australia, and the southern Amazon Rainforest are near the end of their rainy seasons.

By June, those places are dry, and Northern Hemisphere tropical locations, including India, Southeast Asia, and Africa south of the Sahara are receiving rain.

Centered on the Pacific Ocean, this animation of monthly average rain rates shows how the tropical rain belt follows the Sun. The tropical rain belt stretches out in a virtually unbroken line across the open ocean. Over land, the line is distorted because of the interaction between the tropical rain belt and monsoons. In places with a monsoon climate, the prevailing winds over land and adjacent ocean areas reverse directions on a seasonal basis. The winds reverse because the land changes temperature more dramatically from season to season than water; the differences in heating alter the patterns of rising and sinking air.

Winds usually blow offshore in winter and onshore in summer—like a daily coastal sea breeze, but on a much larger scale. For instance, the shifting of the tropical rain belt into the Northern Hemisphere in May and June coincides with the onset of the summer monsoon in Southeast Asia. As summer days lengthen and heating increases, land surfaces what wind belt is closest to the equator the continent of Asia get hotter than surrounding oceans. The land heats the air, and the air rises.

Warm, moist air from the Indian Ocean flows onshore, bringing rain. The interaction between the monsoon and the Inter-tropical Convergence Zone produces heavy rain over India, Southeast Asia, and southeastern China throughout how to overcome culture barriers of the Northern Hemisphere summer.

Similar interactions between monsoons and the north-south migration of tropical rains occurs in Australia, in the Amazon basin of northern South America, West Africa, and in Mexico and the U. Accessed April 19, Marshall, J. London: Elsevier Academic Press. Inter-tropical Convergence Zone. Vanichkajorn, T, and Archevarahuprok, B. Caption by Rebecca Lindsey and Caityln Kennedy.

Skip to main content. Annual Migration of Tropical Rain Belt. Rebecca Lindsey. Caitlyn Kennedy. May 4, This tropical rain belt stretches out in a virtually unbroken line across the open ocean. Over land, the line is distorted because of the interaction between the tropical rain belt and monsoon circulations.

The tropical rain belt migrates north and south of the equator as the seasons change, leading to pronounced wet and dry seasons in many tropical countries. Share This:. Intertropical Convergence Zone. Atmospheric Circulation. Ocean and Climate. Water Cycle. Cyclical and Natural Changes. Measurements and Observations.

How the Climate System Works. Natural Climate Patterns. Understanding Climate. You Might Like. Torrential Rains in Thailand. April 22, Shifting ocean surface saltiness from July 28, September 1, February 5,

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Which wind belt occurs at about about 5 degrees north and south of the equator? doldrums - Wind blows from poles toward the equator. - Wind is created the same way as during a sea breeze. close to the poles in the middle latitude toward the equator in the upper atmosphere.

The Hadley cell , named after George Hadley , is a global scale tropical atmospheric circulation that features air rising near the Equator, flowing poleward at a height of 10 to 15 kilometers above the earth's surface, descending in the subtropics, and then returning equatorward near the surface. This circulation creates the trade winds , tropical rain-belts and hurricanes , subtropical deserts and the jet streams. Hadley cells are the low-altitude overturning circulation that have air sinking at roughly zero to 30 degree latitude.

The driving force of atmospheric circulation is the uneven distribution of solar heating across the Earth, which is greatest near the equator and least at the poles. The atmospheric circulation transports energy polewards, thus reducing the resulting equator-to-pole temperature gradient.

The mechanisms by which this is accomplished differ in tropical and extratropical latitudes. Hadley cells exist on either side of the equator. Each cell encircles the globe latitudinally and acts to transport energy from the equator to about the 30th latitude.

The circulation exhibits the following phenomena: [1]. The Hadley circulation exhibits seasonal variation. During the solstitial seasons DJF and JJA , the upward branch of the Hadley cell occurs not directly over the equator but rather in the summer hemisphere. In the annual mean, the upward branch is slightly offset into the northern hemisphere, making way for a stronger Hadley cell in the southern hemisphere. This evidences a small net energy transport from the northern to the southern hemisphere.

The Hadley system provides an example of a thermally direct circulation. The thermodynamic efficiency of the Hadley system, considered as a heat engine, has been relatively constant over the — period, averaging 2.

Over the same interval, the power generated by the Hadley regime has risen at an average rate of about 0. Overall, the mean meridional circulation cells such as the Hadley circulation are not particularly efficient at reducing the equator-to-pole temperature gradient due to cancellation between transports of different types of energy.

In the Hadley cell, both sensible and latent heat are transported equatorward near the surface, while potential energy is transported above in the opposite direction, poleward. This is partly a result of the strong constraints imposed on atmospheric motions by the conservation of angular momentum. In the early 18th century, George Hadley , an English lawyer and amateur meteorologist , was dissatisfied with the theory that the astronomer Edmond Halley had proposed for explaining the trade winds.

What was no doubt correct in Halley's theory was that solar heating creates upward motion of equatorial air, and air mass from neighboring latitudes must flow in to replace the risen air mass. But for the westward component of the trade winds Halley had proposed that in moving across the sky the Sun heats the air mass differently over the course of the day.

Hadley was not satisfied with that part of Halley's theory and rightly so. Hadley was the first to recognize that Earth's rotation plays a role in the direction taken by an air mass as it moves relative to the Earth. Hadley's theory, published in , remained unknown, but it was rediscovered independently several times.

Among the re-discoverers was John Dalton , who later learned of Hadley's priority. Over time the mechanism proposed by Hadley became accepted, and over time his name was increasingly attached to it. By the end of the 19th century it was shown that Hadley's theory was deficient in several respects. One of the first who accounted for the dynamics correctly was William Ferrel. It took many decades for the correct theory to become accepted, and even today Hadley's theory can still be encountered occasionally, particularly in popular books and websites.

The region in which the equatorward moving air masses converge and rise is known as the intertropical convergence zone , or ITCZ. Within that zone develops a band of thunderstorms that produce high-precipitation.

Having lost most of its water vapor to condensation and precipitation in the upward branch of the Hadley cell circulation, the descending air is dry not wet. As the air descends, low relative humidities are produced as the air is warmed adiabatically by compression from the overlying air, producing a region of higher pressure. The subtropics are relatively free of the convection, or thunderstorms, that are common in the equatorial belt.

Many of the world's deserts are located in these subtropical latitudes. However the deserts do not extend to the eastern side of the various continents because of ocean currents caused by the Trade Winds. The majority of Earth's arid regions are located in the areas beneath the descending part of the Hadley circulation at around 30 degrees latitude. This might lead to large changes in precipitation in the latitudes at the edge of the cells. The hypothesis, that a decline in solar activity reduces the latitudinal extent of the Hadley Circulation and decreases mid-latitudinal monsoon intensity, is matched by data, showing increased dryness in central west Africa and increase in precipitation in temperate zones north.

Meanwhile, mid-latitudinal storm tracks in the temperate zones increased and moved equatorward. From Wikipedia, the free encyclopedia.

Equatorial atmospheric phenomenon. Global physical climatology. ISBN OCLC McElroy Journal of Climate. Bibcode : JCli History of Meteorology. Archived from the original PDF on Retrieved Frierson; Jian Lu; Gang Chen Geophysical Research Letters. Bibcode : GeoRL.. Diaz; Martin P. Hoerling In Henry F. Diaz; Raymond S. Bradley eds. Advances in Global Change Research. Springer Netherlands. Seidel; Qian Fu; William J. Randel; Thomas J. Reichler Nature Geoscience. Bibcode : NatGe Johanson; Qiang Fu CiteSeerX In Issar, A.

Kluwer Academic Publishers, Dordrecht. CS1 maint: multiple names: authors list link. Categories : Tropical meteorology Oceanography. Hidden categories: CS1 maint: multiple names: authors list Articles with short description Short description is different from Wikidata.

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