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contributor authorDalziel, Stuart B.
date accessioned2017-06-09T14:50:24Z
date available2017-06-09T14:50:24Z
date copyright1992/10/01
date issued1992
identifier issn0022-3670
identifier otherams-27931.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164991
description abstractThe functional formalism of Gill and Dalziel is extended for two-layer flows in nonrectangular cross sections. Exchange flow through channels with a range of different cross sections is investigated in detail. Hydraulic transitions are found to play the same role in controlling the flow as in channels with rectangular cross sections. The response of the flow to different alongchannel geometries and net flow rates is qualitatively similar to that for rectangular cross sections but exhibits a number of novel features. In a channel of constant center line depth, the two hydraulic transitions do not coincide at the narrowest point unless the channel is symmetric about its middepth plane. For flow over a sill, the location of the virtual control is found to be a discontinuous function of the net flow rate, undergoing one or two jumps in position (depending on the precise geometry) as the net flow is altered. In the absence of friction and instabilities, it is not possible to eliminate the lower layer from the contraction by increasing the strength of the net flow out of the less dense reservoir if the channel narrows to a point at its bottom.
publisherAmerican Meteorological Society
titleMaximal Exchange in Channels with Nonrectangular Cross Sections
typeJournal Paper
journal volume22
journal issue10
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1992)022<1188:MEICWN>2.0.CO;2
journal fristpage1188
journal lastpage1206
treeJournal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 010
contenttypeFulltext


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