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

机译:干旱和夏季季风过多期间印度地区的降水-气溶胶关系

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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 run. 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.
机译:这项研究基于MODIS(中等分辨率成像分光辐射仪)在550运行时得出的气溶胶光学深度(AOD),调查了印度夏季风期间的气溶胶-降雨相互作用,并表征了它们在干旱和夏季季风过量期间的差异。已使用2级MODIS Terra Data版本6估算了AOD。印度的干旱年AOD高于季风年。气溶胶的总作用导致夏季降水减少,但由于云,辐射,大尺度环流和对流的变化,在夏季季风强弱年中,气溶胶的影响差异明显。气溶胶和云特征与年际尺度上的降雨变化密切相关。发现云有效半径和云光学厚度的变化与气溶胶效应一致。

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