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contributor authorRomps, David M.
date accessioned2017-06-09T16:56:11Z
date available2017-06-09T16:56:11Z
date copyright2012/12/01
date issued2012
identifier issn0022-4928
identifier otherams-76707.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4219184
description abstracthe Gregory?Kershaw?Inness (GKI) parameterization of convective momentum transport, which has a tunable parameter C, is shown to be identical to a parameterization with no pressure gradient force and a mass flux smaller by a factor of 1 ? C. Using cloud-resolving simulations, the transilient matrix for momentum is diagnosed for deep convection in radiative?convective equilibrium. Using this transilient matrix, it is shown that the GKI scheme underestimates the compensating subsidence of momentum by a factor of 1 ? C, as predicted. This result is confirmed using a large-eddy simulation.
publisherAmerican Meteorological Society
titleOn the Equivalence of Two Schemes for Convective Momentum Transport
typeJournal Paper
journal volume69
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS-D-12-068.1
journal fristpage3491
journal lastpage3500
treeJournal of the Atmospheric Sciences:;2012:;Volume( 069 ):;issue: 012
contenttypeFulltext


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