海陆风辐合和地形抬升是海南低槽类冰雹发生的主要触发机制。
The convergence line caused by sea-land breeze and the topographic forcing effect are the main mechanism that triggers the low-trough type hail in Hainan.
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。
For the integrated effects, the raising of TP has little influence on the surface sensible heat flux, while it greatly affects condensation heating.
除迎风坡空气抬升和背风坡引起上升运动外，还有地形加热引起的上升运动，这些对水汽、能量等的垂直输送起着重要作用。
Besides, topographic heating, air lifting on windward slope and lee wave play an important role in vertical transport of moisture and energy.
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