Because of the Earth's surface is unevenly heated, there are big differences in air temperature from the equator to the poles and over different types of terrain . These temperature differences are what cause convection in the atmospheric and air to circulate over the globe.
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This pattern, called atmospheric circulation, is caused because the Sun heats the Earth more at the equator than at the poles. It's also affected by the spin ...
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The Earth's weather is a consequence of its illumination by the Sun and the laws of thermodynamics. The atmospheric circulation can be viewed as a heat engine ... Latitudinal circulation features · Longitudinal circulation features · Walker circulation
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On average, this circulation corresponds to large-scale wind systems arranged in several east–west belts that encircle the Earth. In the subtropical high- ...
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The reason we have different weather patterns, jet streams, deserts and prevailing winds is all because of the global atmospheric circulation caused by the ...
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As air rises, pressure falls and the air cools. As cooler air can hold less moisture, condensation occurs. Therefore in these regions clouds form and ...
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The two major causes of global wind circulation are inequalities in radiation distribution over the Earth's surface and the Earth's rotation.
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Global atmospheric circulation creates winds across the planet as air moves from areas of high pressure to areas of low pressure. It also leads to areas of ...
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13 May 2019 · From synoptic climatology's point of view, a question can be posed: is this warming caused by changes in the frequency of particular circulation ...
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It then moves towards the equator. At 60° the combination of warm and cold air causes the warm air to rise, resulting in low air pressure at 60°. At 60° ...
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Air circulation is caused by the sun heating the earth (and air) as the earth rotates. Different parts of the earth have different thermal characteristics ...
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The reason we have global wind patterns is ultimately due to a differentially heated, rotating Earth. The differential heating of Earth continually causes an ...
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Temperature and water content of air affect its density; Warm air is less dense than cold air; Convection cell: Warm air rises, when it is cooled it sinks back ...
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Differential heating causes air to rise in the atmosphere at some locations on the planet and then to sink back to Earth's surface at other locations.
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The atmospheric circulation in low latitudes corresponds mainly to direct thermal circulations driven by convection over the regions with the highest surface ...
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