高原夏季风强(弱)时，印度全区及我国华北地区容易出现降水偏少(多)。
When the TPSM is strong (weak), the precipitation in all India and North China tends to be less (more) than normal.
结果表明，高原夏季风、长江上游夏季气温和降水均存在明显的阶段性变化特征。
Results show that the Plateau summer monsoon, the summer temperature and precipitation in the upper reach of Changjiang river valley exist obvious change in phase.
高原季风异常可能与高原下垫面热力异常有关，从而推测冬季风异常通过高原这个巨大的热载体而影响夏季风异常。
It is suggested that the monsoon abnormity in plateau is affected by the special surface thermotics which is the media of winter monsoon abnormity leading to summer monsoon abnormity.
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