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contributor authorGrimshaw, Roger
contributor authorBroutman, Dave
contributor authorSahl, Lauren E.
date accessioned2017-06-09T14:48:29Z
date available2017-06-09T14:48:29Z
date copyright1987/08/01
date issued1987
identifier issn0022-3670
identifier otherams-27210.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164191
description abstractAn analytical model is developed for nondivergent barotropic flow in a rectangular region, with depth contours parallel to the longshore boundary. The model is linear, with flow forced by wind stress and subject to dissipation by bottom stress. The friction due to the bottom stress is parameterized by a single friction coefficient, which represents a gross decay time for the whole region. Analytical solutions are developed in detail for a steady or periodic wind stress, which is independent of the cross-shelf coordinate. Results are presented for a range of values of the region dimension and the friction coefficient. Comparisons are made between the analytical model and recent observations of the wind-driven flow in the northern Great Barrier Reef.
publisherAmerican Meteorological Society
titleA Nondivergent Barotropic Model for Wind-Driven Circulation in a Closed Region
typeJournal Paper
journal volume17
journal issue8
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1987)017<1114:ANBMFW>2.0.CO;2
journal fristpage1114
journal lastpage1127
treeJournal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 008
contenttypeFulltext


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