A parameterization of warm clouds for use in atmospheric general circulation models

Simple parameterizations of droplet effective radius in stratiform and convective clouds for use in global climate models are presented. Evidence suggests that a simple relationship exists between droplet effective radius and liquid water content in layer clouds with the droplet effective radius pro...

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Published in:Journal of the atmospheric sciences 1994-10, Vol.51 (19), p.2722-2732
Main Authors: BOWER, K. N, CHOULARTON, T. W, LATHAM, J, NELSON, J, BAKER, M. B, JENSEN, J
Format: Article
Language:English
Subjects:
Atmosphere
Atmospheric circulation
Climate
Climate models
Cloud physics
Clouds
Earth, ocean, space
Exact sciences and technology
External geophysics
Global climate
Meteorology
Rain
Water content
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container_end_page 2732
container_issue 19
container_start_page 2722
container_title Journal of the atmospheric sciences
container_volume 51
creator BOWER, K. N
CHOULARTON, T. W
LATHAM, J
NELSON, J
BAKER, M. B
JENSEN, J
description Simple parameterizations of droplet effective radius in stratiform and convective clouds for use in global climate models are presented. Evidence suggests that a simple relationship exists between droplet effective radius and liquid water content in layer clouds with the droplet effective radius proportional to the cube root of the liquid water content.
doi_str_mv 10.1175/1520-0469(1994)051<2722:apowcf>2.0.co;2
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subjects Atmosphere
Atmospheric circulation
Climate
Climate models
Cloud physics
Clouds
Earth, ocean, space
Exact sciences and technology
External geophysics
Global climate
Meteorology
Rain
Water content
title A parameterization of warm clouds for use in atmospheric general circulation models
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