Ice-ocean boundary conditions for coupled models. Ocean Modelling 7
Abstract. Coupled general circulation models are be-coming more sophisticated, particularly with respect to the sea ice component and the increasing use of free sur-face formulations in the ocean. It is therefore timely to revisit the boundary conditions at the sea ice-ocean in-terface to ensure tha...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.505.644 2023-05-15T18:16:27+02:00 Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 Gavin A. Schmidt Cecilia M. Bitz Uwe Mikolajewicz L. -bruno Tremblay The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.644 http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.644 http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf text 2004 ftciteseerx 2016-01-08T09:21:38Z Abstract. Coupled general circulation models are be-coming more sophisticated, particularly with respect to the sea ice component and the increasing use of free sur-face formulations in the ocean. It is therefore timely to revisit the boundary conditions at the sea ice-ocean in-terface to ensure that a) mass and energy are conserved, b) the physics represented is as realistic as possible, and c) numerical instabilities are avoided. We present here an overview of recent practice from the GISS, NCAR CCSM2.0 and MPI Hamburg coupled models. A new formulation of the basal sea ice °uxes, discussions of lateral melt and snow-ice formation, coupling strategies for the sea ice dynamics component, and interactions with dynamic free surfaces are presented. 1. Text Sea ice Unknown |
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English |
description |
Abstract. Coupled general circulation models are be-coming more sophisticated, particularly with respect to the sea ice component and the increasing use of free sur-face formulations in the ocean. It is therefore timely to revisit the boundary conditions at the sea ice-ocean in-terface to ensure that a) mass and energy are conserved, b) the physics represented is as realistic as possible, and c) numerical instabilities are avoided. We present here an overview of recent practice from the GISS, NCAR CCSM2.0 and MPI Hamburg coupled models. A new formulation of the basal sea ice °uxes, discussions of lateral melt and snow-ice formation, coupling strategies for the sea ice dynamics component, and interactions with dynamic free surfaces are presented. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Gavin A. Schmidt Cecilia M. Bitz Uwe Mikolajewicz L. -bruno Tremblay |
spellingShingle |
Gavin A. Schmidt Cecilia M. Bitz Uwe Mikolajewicz L. -bruno Tremblay Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
author_facet |
Gavin A. Schmidt Cecilia M. Bitz Uwe Mikolajewicz L. -bruno Tremblay |
author_sort |
Gavin A. Schmidt |
title |
Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
title_short |
Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
title_full |
Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
title_fullStr |
Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
title_full_unstemmed |
Ice-ocean boundary conditions for coupled models. Ocean Modelling 7 |
title_sort |
ice-ocean boundary conditions for coupled models. ocean modelling 7 |
publishDate |
2004 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.644 http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.644 http://www.atmos.washington.edu/~bitz/iceocnbcs.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766190083009937408 |