Large-eddy simulations of strongly precipitating, shallow, stratocumulus-topped boundary layers

Large-eddy simulations that incorporate a size-resolving representation of cloud water are used to study the effect of heavy drizzle on PBL structure. Simulated surface precipitation rates average about 1 mm day-1.

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Published in:Journal of the atmospheric sciences 1998-12, Vol.55 (24), p.3616-3638
Main Authors: STEVENS, B, COTTON, W. R, FEINGOLD, G, MOENG, C.-H
Format: Article
Language:English
Subjects:
Atmosphere
Boundary layers
Clouds
Convection, turbulence, diffusion. Boundary layer structure and dynamics
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Rain
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container_end_page 3638
container_issue 24
container_start_page 3616
container_title Journal of the atmospheric sciences
container_volume 55
creator STEVENS, B
COTTON, W. R
FEINGOLD, G
MOENG, C.-H
description Large-eddy simulations that incorporate a size-resolving representation of cloud water are used to study the effect of heavy drizzle on PBL structure. Simulated surface precipitation rates average about 1 mm day-1.
doi_str_mv 10.1175/1520-0469(1998)055<3616:lesosp>2.0.co;2
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1520-0469
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subjects Atmosphere
Boundary layers
Clouds
Convection, turbulence, diffusion. Boundary layer structure and dynamics
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Rain
title Large-eddy simulations of strongly precipitating, shallow, stratocumulus-topped boundary layers
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