= Atmospheric circulation
{wiki=Atmospheric_circulation}
Atmospheric circulation refers to the large-scale movement of air in the Earth's atmosphere, which is driven by differences in solar heating and the rotation of the Earth. This circulation is fundamental to weather patterns and climate systems around the globe. The primary features of atmospheric circulation include: 1. **Hadley Cells**: These are tropical atmospheric circulation cells that extend from the equator to about 30 degrees latitude.
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