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.

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。

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For the integrated effects, the raising of TP has little influence on the surface sensible heat flux, while it greatly affects condensation heating.

高原效应的综合影响方面：地形抬升对地面感热通量的影响较小，对凝结潜热的影响明显。

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