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AGU: Geophysical Research Letters

 

Keywords

  • precipitation
  • tropical meteorology
  • remote sensing

Index Terms

  • Atmospheric Composition and Structure: Cloud optics
  • Atmospheric Composition and Structure: Cloud physics and chemistry
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Global Change: Oceans
  • Global Change: Remote sensing

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L09811, 5 PP., 2007
doi:10.1029/2007GL029335

Tropical oceanic cloudiness and the incidence of precipitation: Early results from CloudSat

John M. Haynes

Department of Atmospheric Science, Colorado State University, Fort Collins, Colorado, USA

Graeme L. Stephens

Department of Atmospheric Science, Colorado State University, Fort Collins, Colorado, USA

Results of analysis of CloudSat radar data collected during the first three months of operation are described. It is shown that the global tropical oceans (30N–30S) predominantly favor clouds with tops in two layers centered at about 2 and 12 km. Precipitating clouds occur primarily in three modes, a shallow mode that is the most frequent type, as well as a middle and deep mode. Regional features are also discussed. The Indian and western Pacific Oceans exhibit more predominantly high clouds and deeper precipitation features than the eastern Pacific and Atlantic. The occurrence of a mid-level mode of cloudiness and precipitation is shown to vary regionally, being particularly significant in the western Pacific. For all regions examined, precipitating clouds are observed to be deeper than non-precipitating clouds. Over the global tropical oceans, 18% of the clouds detected by CloudSat produce precipitation.

Received 12 January 2007; accepted 5 April 2007; published 10 May 2007.

Citation: Haynes, J. M., and G. L. Stephens (2007), Tropical oceanic cloudiness and the incidence of precipitation: Early results from CloudSat, Geophys. Res. Lett., 34, L09811, doi:10.1029/2007GL029335.

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