What reasons for planetary winds?
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The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations.
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They are steady winds lying between 5°N-30°N in the northern hemisphere and 5°S-30°S in the southern hemisphere. The trade winds in the Northern-Hemisphere blow from the north-east direction due to the deflection of the wind caused by the rotation of the Earth and so are called North-East Trades.
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