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.
东南亚地区的夏季风在亚洲季风系统中首先爆发后，通过风场与对流场的变化对周边地区造成影响。
After it first breaks out over the Southeast Asia in the Asian summer monsoon system, summer monsoon over the Southeast Asia affects the peripheral area with varied wind field and convection field.
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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