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contributor authorBennett, John R.
date accessioned2017-06-09T14:44:55Z
date available2017-06-09T14:44:55Z
date copyright1978/11/01
date issued1978
identifier issn0022-3670
identifier otherams-25873.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162704
description abstractA 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.
publisherAmerican Meteorological Society
titleA Three-Dimensional Model of Lake Ontario's Summer Circulation. II. A Diagnostic Study
typeJournal Paper
journal volume8
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1978)008<1095:ATDMOL>2.0.CO;2
journal fristpage1095
journal lastpage1103
treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 006
contenttypeFulltext


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