强降水常出现在台风前进方向的右前侧，相同的垂直累积液态水含量受地形等因素影响“降水效率”差异极大。
Because of the impacts of topography, there is very different precipitation even though the vertically integrated liquid water in the same.
讨论了水汽总量和云中液态水含量的统计反演法以及水汽垂直分布的迭代反演法。
A statistical method for retrieving the total water vapor and cloud liquid water content and a non-linear iterative algorithm for retrieving the water vapor profiles in the troposphere are discussed.
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