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Record #112780:

Numerical simulation of the ice-ocean circulation in the Arctic-GIN sea basin / S. Piacsek, Richard Allard, A. Warn-Varnas.

Title: Numerical simulation of the ice-ocean circulation in the Arctic-GIN sea basin / S. Piacsek, Richard Allard, A. Warn-Varnas.
Author(s): Piacsek, S.
Allard, Richard.
Warn-Varnas, A.
Date: 1991.
In: Eos : transactions, American Geophysical Union. (1991.), Vol. 72(51, supplement) (1991)
Abstract: Abstract presented at AGU 1992 Ocean Sciences Meeting, 27-31 January, New Orleans, LA. Simulations carried out for 1966-90, using 6-h atmospheric forcing fluxes. Ice circulation is described by Hibler ice model, coupled in ocean to turbulent mixed-layer model and diagnostic geostrophic currents. Large interannual variations occur in drift patterns, particularly in winter. Ocean circulation studied by 1-layer reduced-gravity and 2-layer hydrodynamic model with topography. Important finding of these models is that to obtain realistic representation of West Spitsbergen Current, resolution of at least 30 km is needed.
Notes:

Eos : transactions, American Geophysical Union. Vol. 72(51, supplement) :75 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.14 -- Floating ice, movement.
551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*615) -- Norwegian Sea.
(*617) -- Greenland Sea and Fram Strait.
(*616) -- Iceland waters.
SPRI record no.: 112780

MARCXML

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245 10 ‡aNumerical simulation of the ice-ocean circulation in the Arctic-GIN sea basin /‡cS. Piacsek, Richard Allard, A. Warn-Varnas.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 75.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(51, supplement) :75 (1991).
520 3# ‡aAbstract presented at AGU 1992 Ocean Sciences Meeting, 27-31 January, New Orleans, LA. Simulations carried out for 1966-90, using 6-h atmospheric forcing fluxes. Ice circulation is described by Hibler ice model, coupled in ocean to turbulent mixed-layer model and diagnostic geostrophic currents. Large interannual variations occur in drift patterns, particularly in winter. Ocean circulation studied by 1-layer reduced-gravity and 2-layer hydrodynamic model with topography. Important finding of these models is that to obtain realistic representation of West Spitsbergen Current, resolution of at least 30 km is needed.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*615) -- Norwegian Sea.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
651 #7 ‡a(*616) -- Iceland waters.‡2udc
700 1# ‡aAllard, Richard.
700 1# ‡aWarn-Varnas, A.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(51, supplement) (1991) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
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