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contributor authorDeardorff, J. W.
date accessioned2017-06-09T17:38:29Z
date available2017-06-09T17:38:29Z
date copyright1976/01/01
date issued1976
identifier issn0021-8952
identifier otherams-9022.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232465
description abstractThe advantages of using Betts' (1973) liquid-water potential temperature (?l) and also a total moisture variable (qw) within a shallow-cloud numerical model are enumerated. The saturation condition is parameterized as a function of these two variables and pressure, and the subgrid-scale buoyancy flux is expressed in terms of the subgrid-scale vertical fluxes of ?l and qw.
publisherAmerican Meteorological Society
titleUsefulness of Liquid-Water Potential Temperature in a Shallow-Cloud Model
typeJournal Paper
journal volume15
journal issue1
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1976)015<0098:UOLWPT>2.0.CO;2
journal fristpage98
journal lastpage102
treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001
contenttypeFulltext


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