Windward DiffusionSource: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 007::page 974Author:Philip, J. R.
DOI: 10.1175/1520-0450(1997)036<0974:WD>2.0.CO;2Publisher: American Meteorological Society
Abstract: Windward 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.
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| contributor author | Philip, J. R. | |
| date accessioned | 2017-06-09T14:06:20Z | |
| date available | 2017-06-09T14:06:20Z | |
| date copyright | 1997/07/01 | |
| date issued | 1997 | |
| identifier issn | 0894-8763 | |
| identifier other | ams-12508.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4147855 | |
| description abstract | Windward 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. | |
| publisher | American Meteorological Society | |
| title | Windward Diffusion | |
| type | Journal Paper | |
| journal volume | 36 | |
| journal issue | 7 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1997)036<0974:WD>2.0.CO;2 | |
| journal fristpage | 974 | |
| journal lastpage | 977 | |
| tree | Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 007 | |
| contenttype | Fulltext |