The Three-Dimensional Current and Surface Wave EquationsSource: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009::page 1978Author:Mellor, George
DOI: 10.1175/1520-0485(2003)033<1978:TTCASW>2.0.CO;2Publisher: American Meteorological Society
Abstract: Surface wave equations appropriate to three-dimensional ocean models apparently have not been presented in the literature. It is the intent of this paper to correct that deficiency. Thus, expressions for vertically dependent radiation stresses and a definition of the Doppler velocity for a vertically dependent current field are obtained. Other quantities such as vertically dependent surface pressure forcing are derived for inclusion in the momentum and wave energy equations. The equations include terms that represent the production of turbulence energy by currents and waves. These results are a necessary precursor for three-dimensional ocean models that handle surface waves together with wind- and buoyancy-driven currents. Although the third dimension has been added here, the analysis is based on the assumption that the depth dependence of wave motions is provided by linear theory, an assumption that is the basis of much of the wave literature.
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contributor author | Mellor, George | |
date accessioned | 2017-06-09T14:55:56Z | |
date available | 2017-06-09T14:55:56Z | |
date copyright | 2003/09/01 | |
date issued | 2003 | |
identifier issn | 0022-3670 | |
identifier other | ams-29922.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4167203 | |
description abstract | Surface wave equations appropriate to three-dimensional ocean models apparently have not been presented in the literature. It is the intent of this paper to correct that deficiency. Thus, expressions for vertically dependent radiation stresses and a definition of the Doppler velocity for a vertically dependent current field are obtained. Other quantities such as vertically dependent surface pressure forcing are derived for inclusion in the momentum and wave energy equations. The equations include terms that represent the production of turbulence energy by currents and waves. These results are a necessary precursor for three-dimensional ocean models that handle surface waves together with wind- and buoyancy-driven currents. Although the third dimension has been added here, the analysis is based on the assumption that the depth dependence of wave motions is provided by linear theory, an assumption that is the basis of much of the wave literature. | |
publisher | American Meteorological Society | |
title | The Three-Dimensional Current and Surface Wave Equations | |
type | Journal Paper | |
journal volume | 33 | |
journal issue | 9 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(2003)033<1978:TTCASW>2.0.CO;2 | |
journal fristpage | 1978 | |
journal lastpage | 1989 | |
tree | Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009 | |
contenttype | Fulltext |