Rohini L. Bhawar 1,2, P.R.C. Rahul3

  • 1 APEC Climate Center, Busan, Korea
  • 2 Department of Atmospheric and Space Sciences, University of Pune, Pune, India
  • 3 Indian Institute of Tropical Meteorology, Pune, India

Received: November 26, 2012
Revised: March 7, 2013
Accepted: March 7, 2013
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Cite this article:
Bhawar, R.L. and Rahul, P. (2013). Aerosol-Cloud-Interaction Variability Induced by Atmospheric Brown Clouds during the 2009 Indian Summer Monsoon Drought. Aerosol Air Qual. Res. 13: 1384-1391.



Contrasting monsoons of 2008 and 2009 provided a test bed to enhance the understanding of the aerosol variability and aerosol-cloud interaction. Vertical aerosol profiles derived from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) are used to delineate the aerosol properties during the two contrasting Indian summer monsoons. We observed a 30–40% increase in the aerosol occurrence frequency (AOF) in lower altitudes (below 6 km) in 2009 and a 5–8% enhancement in AOF at higher altitudes in 2008. The cloud occurrence frequency also showed more deep convective clouds in 2008 (13–15%) than in 2009. Cloud Fraction, Aerosol Optical Depth and TRMM precipitation data sets have been also used to investigate the aerosol-cloud interaction. We define the microphysical effect as the increase in cloud fraction with increase in aerosols (CCN) and the radiative effect as the decrease of cloud fraction with increase in aerosol loading. We observe a stronger microphysical effect than the radiative effect in 2008 as compared to 2009. In 2009, atmospheric brown clouds were observed from March to September, which slowed down the microphysical effect and enhanced the radiative effect. This resulted in a 30% reduction in the total cloud fraction that may have reduced precipitation, and invigorated the drought conditions during 2009.

Keywords: Atmospheric aerosols; Aerosol optical depth; Atmospheric chemistry; Air pollution; Remote sensing; Cloud aerosol interactions

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