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Record #191457:

Modeling wind-driven circulation and landfast ice-edge processes during polynya events in northern Baffin Bay / Dany Dumont, Yves Gratton, Todd Arbetter.

Title: Modeling wind-driven circulation and landfast ice-edge processes during polynya events in northern Baffin Bay / Dany Dumont, Yves Gratton, Todd Arbetter.
Author(s): Dumont, Dany.
Gratton, Yves.
Arbetter, Todd.
Date: 2010.
In: Journal of Physical Oceanography. (2010.), Vol. 40(6) (2010)
Abstract: Reports development of high-resolution sea ice-ocean numerical model of North Water polynya to study wind-driven circulation during polynya events. Idealised three-layer stratified ocean is used to initialise model to characterise baroclinic response to realistic wind and ice conditions. Modelled general circulation pattern is mainly forced by "along-channel" sea level gradient between Arctic Ocean and Baffin Bay, which determines magnitude of southward Baffin Current, and by "across-channel" sea level gradient in Baffin Bay, which drives northward West Greenland Current.
Notes:

Journal of Physical Oceanography. Vol. 40(6) :1356-1372 (2010).

Keywords: 519.673 -- Modelling.
551.326 -- Floating ice.
551.326.31 -- Polynyas.
551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*60) -- Arctic Ocean and adjacent waters.
(*62) -- Canadian Arctic waters.
(*624) -- Baffin Bay and Davis Strait.
SPRI record no.: 191457

MARCXML

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100 1# ‡aDumont, Dany.
245 10 ‡aModeling wind-driven circulation and landfast ice-edge processes during polynya events in northern Baffin Bay /‡cDany Dumont, Yves Gratton, Todd Arbetter.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2010.
300 ## ‡ap. 1356-1372 :‡bill., diags., tables, maps.
500 ## ‡aJournal of Physical Oceanography. Vol. 40(6) :1356-1372 (2010).
520 3# ‡aReports development of high-resolution sea ice-ocean numerical model of North Water polynya to study wind-driven circulation during polynya events. Idealised three-layer stratified ocean is used to initialise model to characterise baroclinic response to realistic wind and ice conditions. Modelled general circulation pattern is mainly forced by "along-channel" sea level gradient between Arctic Ocean and Baffin Bay, which determines magnitude of southward Baffin Current, and by "across-channel" sea level gradient in Baffin Bay, which drives northward West Greenland Current.
530 ## ‡aAlso issued online ‡uurn:doi:10.1175/2010JPO4292.1‡uhttps://dx.doi.org/10.1175/2010JPO4292.1
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.31 -- Polynyas.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*62) -- Canadian Arctic waters.‡2udc
651 #7 ‡a(*624) -- Baffin Bay and Davis Strait.‡2udc
700 1# ‡aGratton, Yves.
700 1# ‡aArbetter, Todd.
773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 40(6) (2010) ‡wSPRI-78712
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