A Large Eddy Simulation Intercomparison Study of Shallow Cumulus ConvectionSource: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 010::page 1201Author:Siebesma, A. Pier
,
Bretherton, Christopher S.
,
Brown, Andrew
,
Chlond, Andreas
,
Cuxart, Joan
,
Duynkerke, Peter G.
,
Jiang, Hongli
,
Khairoutdinov, Marat
,
Lewellen, David
,
Moeng, Chin-Hoh
,
Sanchez, Enrique
,
Stevens, Bjorn
,
Stevens, David E.
DOI: 10.1175/1520-0469(2003)60<1201:ALESIS>2.0.CO;2Publisher: American Meteorological Society
Abstract: This paper reports an intercomparison study on undisturbed trade wind cumulus convection under steady-state conditions as observed during the Barbados Oceanographic and Meteorological Experiment (BOMEX) with 10 large eddy simulation (LES) models. A main objective of this study is to obtain a quantitative assessment of the quality of the turbulent dynamics for this type of boundary layer clouds as produced by the different LES codes. A 6-h simulation shows excellent model-to-model agreement of the observed vertical thermodynamical structure, reasonable agreement of variances and turbulent fluxes, and good agreement of quantities conditionally sampled within the model clouds, such as cloud cover, liquid water, and cloud updraft strength. In the second part of this paper the LES dataset is used to evaluate simple models that are used in parameterizations of current general circulation models (GCMs). Finally, the relation of this work to subsequent LES studies of more complicated regimes is discussed, and guidance is given for the design of future observational studies of shallow cumulus boundary layers.
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contributor author | Siebesma, A. Pier | |
contributor author | Bretherton, Christopher S. | |
contributor author | Brown, Andrew | |
contributor author | Chlond, Andreas | |
contributor author | Cuxart, Joan | |
contributor author | Duynkerke, Peter G. | |
contributor author | Jiang, Hongli | |
contributor author | Khairoutdinov, Marat | |
contributor author | Lewellen, David | |
contributor author | Moeng, Chin-Hoh | |
contributor author | Sanchez, Enrique | |
contributor author | Stevens, Bjorn | |
contributor author | Stevens, David E. | |
date accessioned | 2017-06-09T14:38:28Z | |
date available | 2017-06-09T14:38:28Z | |
date copyright | 2003/05/01 | |
date issued | 2003 | |
identifier issn | 0022-4928 | |
identifier other | ams-23386.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4159941 | |
description abstract | This paper reports an intercomparison study on undisturbed trade wind cumulus convection under steady-state conditions as observed during the Barbados Oceanographic and Meteorological Experiment (BOMEX) with 10 large eddy simulation (LES) models. A main objective of this study is to obtain a quantitative assessment of the quality of the turbulent dynamics for this type of boundary layer clouds as produced by the different LES codes. A 6-h simulation shows excellent model-to-model agreement of the observed vertical thermodynamical structure, reasonable agreement of variances and turbulent fluxes, and good agreement of quantities conditionally sampled within the model clouds, such as cloud cover, liquid water, and cloud updraft strength. In the second part of this paper the LES dataset is used to evaluate simple models that are used in parameterizations of current general circulation models (GCMs). Finally, the relation of this work to subsequent LES studies of more complicated regimes is discussed, and guidance is given for the design of future observational studies of shallow cumulus boundary layers. | |
publisher | American Meteorological Society | |
title | A Large Eddy Simulation Intercomparison Study of Shallow Cumulus Convection | |
type | Journal Paper | |
journal volume | 60 | |
journal issue | 10 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(2003)60<1201:ALESIS>2.0.CO;2 | |
journal fristpage | 1201 | |
journal lastpage | 1219 | |
tree | Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 010 | |
contenttype | Fulltext |