根据前冬南海海温预测1998年南海夏季风爆发的时间和强度与实际相符。

Prediction of the onset of 1998 'SCSSM based on SST during the prior period in SCS is consistent with the fact.

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结果发现，中纬度高原的感热加热所造成的经、纬向热力差异是导致亚洲夏季风爆发的原因。

Results show that the longitudinal and latitudinal thermal contrasts caused by the middle latitude Plateau sensible heating trigger the onset of the Asian summer monsoon.

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通过进一步的诊断，揭示了亚洲夏季风降水在印度季风区出现较晚以及印度夏季风爆发的动力机制。

Further dynamic analysis reveals the dynamic mechanism for the late occurrence of ASM precipitation in Indian monsoon area and the abrupt occurrence of Indian summer monsoon onset.

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