Circulation
Atmospheric circulation is the large-scale movement of air through the troposphere, and the means (with ocean circulation) by which heat is distributed around the Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic structure remains fairly constant as it is determined by the Earth's rotation rate and the difference in solar radiation between the equator and poles.
Read more about this topic: Earth's Atmosphere
Famous quotes containing the word circulation:
“Tourism, human circulation considered as consumption ... is fundamentally nothing more than the leisure of going to see what has become banal.”
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