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contributor authorArdhuin, Fabrice
contributor authorJenkins, Alastair D.
contributor authorBelibassakis, Konstadinos A.
date accessioned2017-06-09T16:20:11Z
date available2017-06-09T16:20:11Z
date copyright2008/06/01
date issued2008
identifier issn0022-3670
identifier otherams-65985.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207270
description abstractThe lowest order sigma-transformed momentum equation given by Mellor takes into account a phase-averaged wave forcing based on Airy wave theory. This equation is shown to be generally inconsistent because of inadequate approximations of the wave motion. Indeed the evaluation of the vertical flux of momentum requires an estimation of the pressure p and coordinate transformation function s to first order in parameters that define the large-scale evolution of the wave field, such as the bottom slope. Unfortunately, there is no analytical expression for p and s at that order. A numerical correction method is thus proposed and verified. Alternative coordinate transforms that allow a separation of wave and mean flow momenta do not suffer from this inconsistency nor do they require a numerical estimation of the wave forcing. Indeed, the problematic vertical flux is part of the wave momentum flux, thus distinct from the mean flow momentum flux, and not directly relevant to the mean flow evolution.
publisherAmerican Meteorological Society
titleComments on “The Three-Dimensional Current and Surface Wave Equations”
typeJournal Paper
journal volume38
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/2007JPO3670.1
journal fristpage1340
journal lastpage1350
treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 006
contenttypeFulltext


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