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contributor authorEnmar, Linda
contributor authorBorenäs, Karin
contributor authorLake, Iréne
contributor authorLundberg, Peter
date accessioned2017-06-09T16:25:23Z
date available2017-06-09T16:25:23Z
date copyright2009/06/01
date issued2009
identifier issn0022-3670
identifier otherams-67585.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209048
description abstractIn a recent paper Girton et al., due to what appears to be a misunderstanding, stated that a critical-flow analysis of the deep-water transport through the Faroe Bank Channel had been undertaken by Lake et al. on the basis of rotating hydraulic theory for a channel of parabolic cross section. In fact, this quoted investigation dealt with a rectangular passage. In the present comment it is demonstrated how the use of parabolic bathymetry leads to significant improvements of the Froude number results.
publisherAmerican Meteorological Society
titleComments on “Is the Faroe Bank Channel Overflow Hydraulically Controlled?”
typeJournal Paper
journal volume39
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/2008JPO4020.1
journal fristpage1534
journal lastpage1538
treeJournal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 006
contenttypeFulltext


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