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contributor authorPhilip, J. R.
date accessioned2017-06-09T14:06:20Z
date available2017-06-09T14:06:20Z
date copyright1997/07/01
date issued1997
identifier issn0894-8763
identifier otherams-12508.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147855
description abstractWindward diffusion (WD) is customarily neglected in convection-diffusion studies, though some work suggests upwind diffusive flux may be significant. Analyses of internal boundary layers produced by a step change in surface concentration of a scalar with and without WD confirm that the effect of WD is indeed negligible. The analysis with WD is, however, needed if an estimate of upwind diffusive flux is required.
publisherAmerican Meteorological Society
titleWindward Diffusion
typeJournal Paper
journal volume36
journal issue7
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1997)036<0974:WD>2.0.CO;2
journal fristpage974
journal lastpage977
treeJournal of Applied Meteorology:;1997:;volume( 036 ):;issue: 007
contenttypeFulltext


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