Oscillatory Bottom Boundary LayersSource: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 011::page 3075Author:Mellor, George
DOI: 10.1175/1520-0485(2002)032<3075:OBBL>2.0.CO;2Publisher: American Meteorological Society
Abstract: A turbulence closure model is applied to the case of an oscillating boundary layer; model calculations compare favorably with data. Wave-induced oscillations can be temporally resolved in a one-dimensional model but not in three-dimensional ocean models, and, indeed, statistical wave models, working in consort with ocean models, can only provide information on expected wave periods and amplitudes. Therefore, in this paper, a way has been found to parameterize the effects of bottom flow oscillations; it entails augmenting the turbulence shear production as a function of amplitude and period of the oscillation, the bottom shear stress of the mean current flow, and the angle between the directions of the oscillations and the mean flow. The more conventional method of solving for an apparent wall roughness is also investigated in an appendix.
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contributor author | Mellor, George | |
date accessioned | 2017-06-09T14:55:30Z | |
date available | 2017-06-09T14:55:30Z | |
date copyright | 2002/11/01 | |
date issued | 2002 | |
identifier issn | 0022-3670 | |
identifier other | ams-29774.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4167038 | |
description abstract | A turbulence closure model is applied to the case of an oscillating boundary layer; model calculations compare favorably with data. Wave-induced oscillations can be temporally resolved in a one-dimensional model but not in three-dimensional ocean models, and, indeed, statistical wave models, working in consort with ocean models, can only provide information on expected wave periods and amplitudes. Therefore, in this paper, a way has been found to parameterize the effects of bottom flow oscillations; it entails augmenting the turbulence shear production as a function of amplitude and period of the oscillation, the bottom shear stress of the mean current flow, and the angle between the directions of the oscillations and the mean flow. The more conventional method of solving for an apparent wall roughness is also investigated in an appendix. | |
publisher | American Meteorological Society | |
title | Oscillatory Bottom Boundary Layers | |
type | Journal Paper | |
journal volume | 32 | |
journal issue | 11 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(2002)032<3075:OBBL>2.0.CO;2 | |
journal fristpage | 3075 | |
journal lastpage | 3088 | |
tree | Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 011 | |
contenttype | Fulltext |