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dc.contributor.authorJacobs, Adrie F. G.
dc.contributor.authorSchols, Emile
dc.date.accessioned2017-06-09T14:01:26Z
dc.date.available2017-06-09T14:01:26Z
dc.date.copyright1986/11/01
dc.date.issued1986
dc.identifier.issn0733-3021
dc.identifier.otherams-11076.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146264
dc.description.abstractThe surface roughness parameter, z0, can be estimated with different techniques. These techniques are analyzing the mean wind profile, estimating the surface drag coefficient and using the universal functions according to the Monin-Obukhov similarity theory. The first two techniques mentioned have been applied over more or less homogeneous terrain. As a result, it appears that the drag method is very sensitive to shear stress measuring errors and to local changes and irregularities in terrain.
dc.publisherAmerican Meteorological Society
dc.titleSurface Roughness Parameter Estimated with a Drag Technique
dc.typeJournal Paper
dc.journal.volume25
dc.journal.issue11
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1986)025<1577:SRPEWA>2.0.CO;2
dc.journal.fristpage1577
dc.journal.lastpage1582
dc.treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011
dc.contenttypeFulltext


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