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.
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.
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。
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