热带气旋降水是台风活动的一个重要体现。
2010年5月，热带气旋“莱拉”给孟加拉湾及印度部分地区带来强劲降水及大风天气。
Tropical Cyclone Laila brought heavy rains and strong winds to the Bay of Bengal and parts of India in May 2010.
改进了热带气旋暴雨的落区及降水强度，且主要落区误差的修正位于热带气旋移动路径的右侧并同主要的SST降温区相关；
The distribution and intensity of mesoscale rainfall are improved, with main distribution correction lying on the right of cyclone track and correlating with SST dropping area.
影响深圳的热带气旋数量减少，但降水强度在加大。
The frequency of the tropical cyclone influencing Shenzhen has decreased, but its impact on heavy rainfall become more serious.
热带气旋北上时，存在第二类间接作用，不仅在东风急流下游能出现倒槽暴雨，还有利于热带气旋下游的副热带高压另一侧产生特大降水。
Second indirect effect is existed when tropical cyclone moves toward the north. The heavy rain-fall of inversion trough has not only arisen in downstream of easter…
热带气旋北上时，存在第二类间接作用，不仅在东风急流下游能出现倒槽暴雨，还有利于热带气旋下游的副热带高压另一侧产生特大降水。
Second indirect effect is existed when tropical cyclone moves toward the north. The heavy rain-fall of inversion trough has not only arisen in downstream of easter…
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