A Three-Dimensional Model of Lake Ontario's Summer Circulation. II. A Diagnostic StudySource: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 006::page 1095Author:Bennett, John R.
DOI: 10.1175/1520-0485(1978)008<1095:ATDMOL>2.0.CO;2Publisher: American Meteorological Society
Abstract: A two-layer circular lake model is used to study the mean flow of Lake Ontario during midsummer. By computing the model only to the second order of amplitude, it is shown that the observed cyclonic circulation of Lake Ontario during summer is due to the rectified effects of the large, transient, wind-driven currents. This effect is strongly influenced by model grid resolution and friction.
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contributor author | Bennett, John R. | |
date accessioned | 2017-06-09T14:44:55Z | |
date available | 2017-06-09T14:44:55Z | |
date copyright | 1978/11/01 | |
date issued | 1978 | |
identifier issn | 0022-3670 | |
identifier other | ams-25873.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162704 | |
description abstract | A two-layer circular lake model is used to study the mean flow of Lake Ontario during midsummer. By computing the model only to the second order of amplitude, it is shown that the observed cyclonic circulation of Lake Ontario during summer is due to the rectified effects of the large, transient, wind-driven currents. This effect is strongly influenced by model grid resolution and friction. | |
publisher | American Meteorological Society | |
title | A Three-Dimensional Model of Lake Ontario's Summer Circulation. II. A Diagnostic Study | |
type | Journal Paper | |
journal volume | 8 | |
journal issue | 6 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1978)008<1095:ATDMOL>2.0.CO;2 | |
journal fristpage | 1095 | |
journal lastpage | 1103 | |
tree | Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 006 | |
contenttype | Fulltext |