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Why is there less winter monsoon than summer monsoon in West Asia?
In summer, southwest winds blow in West Asia, which is generally formed by the southeast trade winds in the southern hemisphere moving northward across the equator. However, the terrain in the southwest of West Asia is dominated by mountainous plateaus, with low latitude and high temperature, prevailing updraft, strong convection and strong wind. The subtropical high control in winter, coupled with the prevailing northeast wind, makes the wind smaller.