Lidar investigations on the structure and microphysical properties of cirrus at a tropical station Gadanki (13.5° N and 79.2° E), India

G. S. Jayeshlal, M. Satyanarayana, G. S. Motty, Reji k. Dhaman, V. Krishnakumar, V. P. Mahadevan Pillai
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Abstract

Cirrus clouds are mainly composed of ice crystals and are known to be the major natural contributors to radiative forcing in the Earth’s atmosphere system. Describing the formation and microphysical properties of cirrus clouds and their role in climate models remain a challenging study. Lidar is a unique instrument, which provides the information on the optical and microphysical properties of cirrus clouds with good spatial and temporal resolutions. In this study we present the microphysical properties of cirrus clouds and their temporal variability, obtained using the ground based dual polarisation lidar at the tropical station Gadanki (13.5° N and 79.2° E), India, during the period January2009 to March 2011. Using the method developed in house for deriving range dependent lidar ratio (LR), the lidar measurements are used for deriving the extinction coefficient and to obtain the nature of the scatterers present in the cloud. It is noted that lidar ratio plays an important role and its measurements indicate directly the type of the ice nucleating aerosol particles present in the cloud. The long term data obtained on the structure of the cirrus in this regard are useful in the climate modelling studies.
印度Gadanki热带站(13.5°N和79.2°E)卷云结构和微物理特性的激光雷达研究
卷云主要由冰晶组成,是地球大气系统辐射强迫的主要自然贡献者。描述卷云的形成和微物理特性及其在气候模式中的作用仍然是一个具有挑战性的研究。激光雷达是一种独特的仪器,可以提供卷云的光学和微物理特性信息,具有良好的空间和时间分辨率。在这项研究中,我们展示了2009年1月至2011年3月期间印度Gadanki热带站(13.5°N和79.2°E)地面双偏振激光雷达获得的卷云微物理特性及其时间变化。利用内部开发的计算距离相关激光雷达比(LR)的方法,激光雷达测量值用于计算消光系数并获得云中存在的散射体的性质。注意到激光雷达比起着重要的作用,其测量结果直接表明云中存在的冰成核气溶胶粒子的类型。在这方面获得的关于卷云结构的长期数据在气候模拟研究中是有用的。
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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