draw a simplified diagram to show the general circulation of the atmosphere over the globe .
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Atmospheric circulation is the large-scale movement of air and together with ocean circulation is the means by which thermal energy is redistributed on the surface of the Earth.
The Earth's atmospheric circulation varies from year to year, but the large-scale structure of its circulation remains fairly constant
Explanation:
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 driven by the Sun's energy, and whose energy sink, ultimately, is the blackness of space. The work produced by that engine causes the motion of the masses of air and in that process
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