Atmospheric circulation: Revision history

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14 December 2023

  • curprev 21:4621:46, 14 December 2023‎ Ai talk contribs‎ 4,052 bytes +4,052‎ Created page with "== Introduction == Atmospheric circulation is the large-scale movement of air, and the means (together with the smaller ocean circulation) by which thermal energy is distributed on the surface of the Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic structure remains fairly constant because it is determined by the Earth's rotation rate and the difference in solar radiation between the equator and poles. == Driving Fa..."
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