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contributor authorRichter, Jadwiga H.
contributor authorSassi, Fabrizio
contributor authorGarcia, Rolando R.
date accessioned2017-06-09T16:28:23Z
date available2017-06-09T16:28:23Z
date copyright2010/01/01
date issued2010
identifier issn0022-4928
identifier otherams-68506.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210072
description abstractMiddle atmospheric general circulation models (GCMs) must employ a parameterization for small-scale gravity waves (GWs). Such parameterizations typically make very simple assumptions about gravity wave sources, such as uniform distribution in space and time or an arbitrarily specified GW source function. The authors present a configuration of the Whole Atmosphere Community Climate Model (WACCM) that replaces the arbitrarily specified GW source spectrum with GW source parameterizations. For the nonorographic wave sources, a frontal system and convective GW source parameterization are used. These parameterizations link GW generation to tropospheric quantities calculated by the GCM and provide a model-consistent GW representation. With the new GW source parameterization, a reasonable middle atmospheric circulation can be obtained and the middle atmospheric circulation is better in several respects than that generated by a typical GW source specification. In particular, the interannual NH stratospheric variability is significantly improved as a result of the source-oriented GW parameterization. It is also shown that the addition of a parameterization to estimate mountain stress due to unresolved orography has a large effect on the frequency of stratospheric sudden warmings in the NH stratosphere by changing the propagation of stationary planetary waves into the polar vortex.
publisherAmerican Meteorological Society
titleToward a Physically Based Gravity Wave Source Parameterization in a General Circulation Model
typeJournal Paper
journal volume67
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2009JAS3112.1
journal fristpage136
journal lastpage156
treeJournal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 001
contenttypeFulltext


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