热带气旋降水是台风活动的一个重要体现。

TC rainfall is a important part of typhoon activity.

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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.

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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.

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