Precipitation-aerosol relationship over the Indian region during drought and excess summer monsoon years

Sajani Surendran, K. Rajendran, Arya V. B.
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引用次数: 1

Abstract

This study investigates the aerosols-rainfall interaction during Indian summer monsoon and characterizes their difference in drought and excess summer monsoon years, based on MODIS (MODerate Resolution Imaging Spectro-radiometer) derived Aerosol Optical Depth (AOD) at 550 nm. AOD has been estimated using Level-2 MODIS Terra Data Version 6. AOD in drought years is found to be higher over India compared to excess monsoon years. The total effect of aerosols causes reduction of summer rainfall but with distinct differences in their impact during strong and weak summer monsoon years, due to the changes in clouds, radiation, large-scale circulation, and convection. Aerosol and cloud characteristics exhibit strong association to rainfall variability in interannual time scales. Variability in cloud effective radius and cloud optical thickness is found to be consistent with aerosol effect.
干旱和过度夏季风年期间印度地区降水-气溶胶关系
本文基于MODIS(中分辨率成像光谱辐射计)在550 nm得到的气溶胶光学深度(AOD),研究了印度夏季风期间气溶胶与降雨的相互作用,并表征了它们在干旱和夏季风年的差异。AOD是使用Level-2 MODIS Terra Data Version 6估算的。干旱年的AOD比季风年高。气溶胶的总效应导致夏季降雨减少,但在强和弱夏季风年,由于云、辐射、大尺度环流和对流的变化,其影响有明显差异。在年际时间尺度上,气溶胶和云特征与降雨变率有很强的相关性。发现云有效半径和云光学厚度的变率与气溶胶效应一致。
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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