4.4 Article

Microphysics of Premonsoon and Monsoon Clouds as Seen from In Situ Measurements during the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX)

Journal

JOURNAL OF THE ATMOSPHERIC SCIENCES
Volume 68, Issue 9, Pages 1882-1901

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/2011JAS3707.1

Keywords

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Funding

  1. Department of Homeland Security of the United States [FY2008-06-16]
  2. Israel Science Foundation [140/07]
  3. Mesoscale Microscale Meteorology Division, National Center for Atmospheric Research (NCAR), United States
  4. Ministry of Earth Sciences, Government of India
  5. Ministry of Earth Sciences, Government of New Delhi

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Analysis of the microphysical structure of deep convective clouds using in situ measurements during the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX) over the Indian peninsular region is presented. It is shown that droplet size distributions (DSDs) in highly polluted premonsoon clouds are substantially narrower than DSDs in less polluted monsoon clouds. High values of DSD dispersion (0.3-0.6) and its vertical variation in the transient and monsoon clouds are related largely to the existence of small cloud droplets with diameters less than 10 mm, which were found at nearly all levels. This finding indicates the existence of a continuous generation of the smallest droplets at different heights. In some cases this generation of small droplets leads to the formation of bimodal and even multimodal DSDs. The formation of bimodal DSDs is especially pronounced in monsoon clouds. Observational evidence is presented to suggest that in-cloud nucleation at elevated layers is a fundamental mechanism for producing multimodal drop size distribution in monsoon clouds as well as in most deep convective clouds. These findings indicate that inclusion of continued nucleation away from the cloud base into numerical models should be considered to predict microphysics and precipitation of clouds in monsoons and other cloud-related phenomena.

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