季风低压是发生在夏季风影响区域的一种低压系统。常把西太平洋和孟加拉湾季风槽中发生的低压专门称为季风低压。
印度季风低压爆发迟、强度弱；
The India monsoon low deepened eruptively later, and its intensity was weaker.
夏季，印度低压和东亚的季风低压均减弱；而副热带高压系统普遍增强。
Indian low and monsoon low of East Asia have the obvious weakness in summer and subtropical high system generally strengthens.
本文用综合方法给出了南海季风低压和南海台风的平均结构，并分别计算了它们的涡度收支。
In this paper by using the composite method the mean structure aud the vorticity budget of the monsoon depression and the typhoon over the South ChinaSea are given.
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