Cloud Liquid Water Derived from Lidar Observations

J. Spinhirne, W. Hart, R. Boers
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Abstract

The distribution of liquid water at the top of clouds has an important relation to the radiative and dynamical interactions within clouds. As a significant example, the formation and structure of marine stratus clouds are maintained primarily by radiative cooling at the cloud top. Understanding the formation of marine stratus is important climatalogically since the cloud type has a significant global influence on the balance between reflected visible and emitted thermal radiation. Models have shown that the interaction between radiative cooling and the cloud development are largley a function of the distribution of the liquid water at the cloud top. Although liquid water may be obtained from in situ measurements, only one dimensional observations are possible. Lidar liquid water observatios can provide a more complete two dimentional representation of the liquid water structure of cloud tops. In this contribution we will describe the lidar retrieval of cloud top liquid water during an experiment in which marine stratus clouds were studied by combined remote sensing and in situ observations.
由激光雷达观测得出的云液态水
云顶液态水的分布与云内的辐射和动力相互作用有重要的关系。作为一个显著的例子,海洋层云的形成和结构主要是通过云顶的辐射冷却来维持的。了解海洋层的形成具有重要的气气学意义,因为云类型对反射的可见光和发射的热辐射之间的平衡具有重要的全球影响。模式表明,辐射冷却和云发展之间的相互作用在很大程度上是云顶液态水分布的函数。虽然可以从原位测量中获得液态水,但只能进行一维观测。激光雷达液态水观测可以提供更完整的云顶液态水结构的二维表示。在这篇文章中,我们将描述在一个结合遥感和原位观测研究海洋层云的实验中,激光雷达对云顶液态水的反演。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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