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Record #140214:

High-resolution simulations of oceanic convection and ice-ocean interactions / Jan O. Backhaus, Jochen Kampf.

Title: High-resolution simulations of oceanic convection and ice-ocean interactions / Jan O. Backhaus, Jochen Kampf.
Author(s): Backhaus, Jan O.,
Kampf, Jochen,
Date: 1996.
Publisher: Cambridge: Sea Ice Group, Scott Polar Research Institute, University of Cambridge
In: ESOP. European Subpolar Ocean Programme. Sea ice - ocean interactions. Volume 2. (1996.),
Abstract: Presents a hypothesis about the Greenland Sea fresh-water layer. Results of two high-resolution convection models are discussed in relation to hydrographic features and ice conditions of the Greenland Sea. One is a 2.5-dimensional model, called SLICE. The second one is a fully three-dimensional convection model, called CUBE. Both models are non-linear and non-hydrostatic and they include all three Coriolis terms. Both are interactively coupled to a thermo-hydrodynamic ice model via fluxes of momentum, heat and salt. From a comparison of both models for the same stratification and forcing we know under which circumstances SLICE produces similar results as CUBE.
Notes:

In: ESOP. European Subpolar Ocean Programme. Sea ice - ocean interactions. Volume 2 / Peter Wadhams, Jeremy P. Wilkinson, Stephen C.S. Wells, eds.

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.46 -- Oceanography, physical.
551.465.4 -- Oceanography, stratification.
001.89 -- Research programmes: European Subpolar Ocean Programme.
C -- Oceanography, hydrography and hydrology.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 140214

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100 1# ‡aBackhaus, Jan O., ‡uDEU-UHa-IM.
245 10 ‡aHigh-resolution simulations of oceanic convection and ice-ocean interactions /‡cJan O. Backhaus, Jochen Kampf.
260 ## ‡aCambridge :‡bSea Ice Group, Scott Polar Research Institute, University of Cambridge,‡c1996.
300 ## ‡ap. 380-436.
500 ## ‡aIn: ESOP. European Subpolar Ocean Programme. Sea ice - ocean interactions. Volume 2 / Peter Wadhams, Jeremy P. Wilkinson, Stephen C.S. Wells, eds.
520 3# ‡aPresents a hypothesis about the Greenland Sea fresh-water layer. Results of two high-resolution convection models are discussed in relation to hydrographic features and ice conditions of the Greenland Sea. One is a 2.5-dimensional model, called SLICE. The second one is a fully three-dimensional convection model, called CUBE. Both models are non-linear and non-hydrostatic and they include all three Coriolis terms. Both are interactively coupled to a thermo-hydrodynamic ice model via fluxes of momentum, heat and salt. From a comparison of both models for the same stratification and forcing we know under which circumstances SLICE produces similar results as CUBE.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc
650 07 ‡a001.89 -- Research programmes: European Subpolar Ocean Programme.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
700 1# ‡aKampf, Jochen, ‡uDEU-UHa-IM.
773 0# ‡7nnam ‡aPeter Wadhams, Jeremy P. Wilkinson, Stephen C.S. Wells, eds. ‡tESOP. European Subpolar Ocean Programme. Sea ice - ocean interactions. Volume 2. ‡dCambridge : Sea Ice Group, Scott Polar Research Institute, University of Cambridge, 1996. ‡wSPRI-139602
917 ## ‡aUnenhanced record from Muscat, imported 2019
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