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。
Surrounding the path is a layer of water two centimetres thick, which is sprayed onto it every seven minutes by nozzles creating a temporary cloud and mist between the mountains.
路线周围还有一层大约两厘米深的水，通过接管这些水每隔七分钟就会蒸发成临时的山间云雾。
The fundamentals and method of deducing path-integrated cloud liquid water content (L)by an airborne up-looking microwave radiometer are introduced in this paper.
本文介绍机载对空微波辐射计探测云中路径积分液态水含量（L）的辐射传输原理和反演方法；
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