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contributor authorGeernaert, Gerald
contributor authorKatsaros, Kristina B.
date accessioned2017-06-09T14:48:02Z
date available2017-06-09T14:48:02Z
date copyright1986/09/01
date issued1986
identifier issn0022-3670
identifier otherams-27062.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164026
description abstractBased on the assumption that, over the sea, the roughness length of the wind profile scales with the wind stress, a new formulation that describes the drag coefficient as a function of the given neutral drag coefficient and stability is derived. The new formulation is compared to an earlier formulation where roughness changes with stability were ignored. The two are then illustrated with data collected from both the Marine Remote Sensing Project (1979) and the Tower Ocean Wave and Radar Dependence Experiment (1984). It was found that when the surface roughness was allowed to depend on wind stress (and therefore stability), the stratification correction to the neutral drag coefficient was larger than for the case when the roughness length was not allowed to vary.
publisherAmerican Meteorological Society
titleIncorporation of Stratification Effects on the Oceanic Roughness Length in the Derivation of the Neutral Drag Coefficient
typeJournal Paper
journal volume16
journal issue9
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1986)016<1580:IOSEOT>2.0.CO;2
journal fristpage1580
journal lastpage1584
treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 009
contenttypeFulltext


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