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.
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.
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