southeast trade wind
Quick Summary
The southeast trade wind is a persistent wind that blows toward the Equator from subtropical high-pressure belts. These winds are stronger and more consistent over oceans than land and were historically crucial for sailing ships crossing westward.1
In meteorology, the trade winds are part of a larger atmospheric circulation pattern known as the Hadley cell. Air descends in subtropical high-pressure regions, then moves towards the Equator. Due to the Coriolis effect, this equatorward flow is deflected, resulting in northeast winds north of the Equator and southeast winds south of it. These winds converge in the intertropical convergence zone (ITCZ), an area near the Equator characterized by rising air, convection, and frequent thunderstorms.234
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