印度低压，又称“亚洲低压”，是亚洲大陆夏季大气活动中心之一。同一纬度地区，夏季大陆形成热低压，冬季大陆形成冷高压。
印度低压偏强并持续稳定。
Indian Low Pressure is more strong and sustainable stability.
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.
对东亚季风气候具有决定性影响的系统，如副热带高压、蒙古高压、印度低压以及西风急流等也模拟得比较好。
The large scale systems such as Subtropical High, Mongolia High, Indian Low which have important influence on the East Asia Monsoon are also simulated pretty well.
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