东南季风,属季风亚洲中的一个季风。盛行于一带,为风向东南的夏季季风。亚洲内陆于夏季时,地面接受太阳热量后,温度迅速增高,形成一广大的低压区,使得太平洋上之空气吹向陆地,这种气流在亚洲被称为“东南季风”。

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