The energy that reaches the Earth's equator is redistributed through air currents and ocean currents.
Atmospheric circulation is a term used in geography to refer to the movement of air on a large scale that serves as the distribution of solar heat on the surface of the Earth.
As a result of the latitudinal circulation, the solar radiation (that affects the low equatorial latitudes) uses air currents, differences in atmospheric pressure and water currents to distribute itself throughout the Earth's atmosphere.
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