Vertically integrated liquid water con 青藏高原东北侧雹云单体最大垂直累积液态含水量的演变特征及其在降雹定时判断中的应用
Because of the impacts of topography, there is very different precipitation even though the vertically integrated liquid water in the same.
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。
Cloud liquid water path (i. e. vertically-integrated cloud liquid water) is an important parameter in meteorology and cloud and mist physics.
云水总量(也可称为液水路径)是一个重要的气象学和云雾物理参数。
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