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Comments on "Is the Faroe Bank Channel owerflow hydraulically controlled"?

Enmar, Linda, 1978- (author)
Stockholms universitet,Meteorologiska institutionen (MISU)
Borenäs, Karin, 1953 (author)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
Lake, Irene (author)
Sveriges meteorologiska och hydrologiska institut, SMHI
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Lundberg, Peter (author)
Stockholms universitet,Meteorologiska institutionen (MISU)
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 (creator_code:org_t)
Boston : American Meteorological Society, 2009
2009
English.
In: Journal of Physical Oceanography. - Boston : American Meteorological Society. - 0022-3670 .- 1520-0485. ; 39:6, s. 1534-1538
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • 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.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)

Keyword

Oceanography
Oceanografi
Oceanography
oceanografi
Hydraulic control
Faroe-Bank Channel

Publication and Content Type

ref (subject category)
art (subject category)

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