contributor author | Enmar, Linda | |
contributor author | Borenäs, Karin | |
contributor author | Lake, Iréne | |
contributor author | Lundberg, Peter | |
date accessioned | 2017-06-09T16:25:23Z | |
date available | 2017-06-09T16:25:23Z | |
date copyright | 2009/06/01 | |
date issued | 2009 | |
identifier issn | 0022-3670 | |
identifier other | ams-67585.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4209048 | |
description abstract | In 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. | |
publisher | American Meteorological Society | |
title | Comments on “Is the Faroe Bank Channel Overflow Hydraulically Controlled?” | |
type | Journal Paper | |
journal volume | 39 | |
journal issue | 6 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/2008JPO4020.1 | |
journal fristpage | 1534 | |
journal lastpage | 1538 | |
tree | Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 006 | |
contenttype | Fulltext | |