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contributor authorGarratt, J. R.
date accessioned2017-06-09T13:58:46Z
date available2017-06-09T13:58:46Z
date copyright1982/05/01
date issued1982
identifier issn0021-8952
identifier otherams-10272.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145371
description abstractThe Zilitenkevitch relation for nocturnal boundary-layer (NBL) depth h in terms of scales u*/f and L is necessarily a poor predictor of h when single-point values of surface fluxes are used. This is because the latter are poor estimates of ensemble-mean fluxes which satisfy this relation. The argument is equally valid both in an evolving and equilibrium NBL.
publisherAmerican Meteorological Society
titleSurface Fluxes and the Nocturnal Boundary-Layer Height
typeJournal Paper
journal volume21
journal issue5
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1982)021<0725:SFATNB>2.0.CO;2
journal fristpage725
journal lastpage729
treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 005
contenttypeFulltext


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