On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model

A finite-element coupled sea ice--ocean model (FESOM) has been developed at the Alfred Wegener Institute for Polar and Marine Research.The sea-ice component is a dynamic-thermodynamic model with an elastic-viscous-plastic rheology.The ocean component is the primitive-equation Finite Element Ocean Mo...

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Main Authors: Timmermann, Ralph, Böning, Carmen, Schröter, Jens, Danilov, Sergey
Format: Conference Object
Language:unknown
Published: 2007
Subjects:
Online Access:https://epic.awi.de/id/eprint/17567/
https://hdl.handle.net/10013/epic.27926
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spelling ftawi:oai:epic.awi.de:17567 2024-09-15T17:36:47+00:00 On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model Timmermann, Ralph Böning, Carmen Schröter, Jens Danilov, Sergey 2007 https://epic.awi.de/id/eprint/17567/ https://hdl.handle.net/10013/epic.27926 unknown Timmermann, R. , Böning, C. , Schröter, J. orcid:0000-0002-9240-5798 and Danilov, S. orcid:0000-0001-8098-182X (2007) On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model , Geophysical Research Abstracts 9, EGU2007-A-07368. . hdl:10013/epic.27926 EPIC3Geophysical Research Abstracts 9, EGU2007-A-07368. Conference notRev 2007 ftawi 2024-06-24T04:00:13Z A finite-element coupled sea ice--ocean model (FESOM) has been developed at the Alfred Wegener Institute for Polar and Marine Research.The sea-ice component is a dynamic-thermodynamic model with an elastic-viscous-plastic rheology.The ocean component is the primitive-equation Finite Element Ocean Model (FEOM).An eight-compartment model of the marine ecosystem, featuring nitrate and silicate cycles and considering possible iron limitation, has been implemented.The coupled model has been configured (1) in a circumpolar domain covering the Southern Ocean between the coast of Antarctica and 48S, and (2) on a global grid with $1.5^\circ$ mean resolution.Multi-decadal simulations have been performed in both configurations using atmospheric forcing data from the NCEP reanalysis. The circumpolar model has also been integrated with atmospheric forcing from the ECHAM5-MPIOM coupled climate model.Results are analysed with regard to ice concentration and thickness, as well as ocean hydrography and circulation.All model setups yield stable integrations and give quite reasonable results. In simulations forced by NCEP reanalysis data, summer ice coverage in the western Weddell Sea is substantially underestimated.This deficiency is cured by using forcing from the ECHAM5-MPIOM simulations, which contain substantially lower temperatures and a different wind pattern in this area.This indicates that the underestimation of ice concentration and thickness in the northwestern Weddell Sea, which is typical to many models of the Southern Ocean, is not due to model deficiences but produced by a poor representation of the Antarctic Peninsula in the NCAR/NCEP reanalysis model.For winter conditions, however, especially outside the peninsula region, NCEP forcing data yield very good results.Results from a wide range of sensitivity studies confirm the crucial importance of a carefully chosen adaptive mixing scheme to parameterize vertical and horizontal mixing.Specifically, to reproduce Southern Ocean hydrography and circulation at the same ... Conference Object Alfred Wegener Institute Antarc* Antarctic Antarctic Peninsula Antarctica Sea ice Southern Ocean Weddell Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description A finite-element coupled sea ice--ocean model (FESOM) has been developed at the Alfred Wegener Institute for Polar and Marine Research.The sea-ice component is a dynamic-thermodynamic model with an elastic-viscous-plastic rheology.The ocean component is the primitive-equation Finite Element Ocean Model (FEOM).An eight-compartment model of the marine ecosystem, featuring nitrate and silicate cycles and considering possible iron limitation, has been implemented.The coupled model has been configured (1) in a circumpolar domain covering the Southern Ocean between the coast of Antarctica and 48S, and (2) on a global grid with $1.5^\circ$ mean resolution.Multi-decadal simulations have been performed in both configurations using atmospheric forcing data from the NCEP reanalysis. The circumpolar model has also been integrated with atmospheric forcing from the ECHAM5-MPIOM coupled climate model.Results are analysed with regard to ice concentration and thickness, as well as ocean hydrography and circulation.All model setups yield stable integrations and give quite reasonable results. In simulations forced by NCEP reanalysis data, summer ice coverage in the western Weddell Sea is substantially underestimated.This deficiency is cured by using forcing from the ECHAM5-MPIOM simulations, which contain substantially lower temperatures and a different wind pattern in this area.This indicates that the underestimation of ice concentration and thickness in the northwestern Weddell Sea, which is typical to many models of the Southern Ocean, is not due to model deficiences but produced by a poor representation of the Antarctic Peninsula in the NCAR/NCEP reanalysis model.For winter conditions, however, especially outside the peninsula region, NCEP forcing data yield very good results.Results from a wide range of sensitivity studies confirm the crucial importance of a carefully chosen adaptive mixing scheme to parameterize vertical and horizontal mixing.Specifically, to reproduce Southern Ocean hydrography and circulation at the same ...
format Conference Object
author Timmermann, Ralph
Böning, Carmen
Schröter, Jens
Danilov, Sergey
spellingShingle Timmermann, Ralph
Böning, Carmen
Schröter, Jens
Danilov, Sergey
On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
author_facet Timmermann, Ralph
Böning, Carmen
Schröter, Jens
Danilov, Sergey
author_sort Timmermann, Ralph
title On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
title_short On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
title_full On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
title_fullStr On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
title_full_unstemmed On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model
title_sort on the representation of the southern ocean in a finite-element coupled sea ice-ocean model
publishDate 2007
url https://epic.awi.de/id/eprint/17567/
https://hdl.handle.net/10013/epic.27926
genre Alfred Wegener Institute
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Sea ice
Southern Ocean
Weddell Sea
genre_facet Alfred Wegener Institute
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Sea ice
Southern Ocean
Weddell Sea
op_source EPIC3Geophysical Research Abstracts 9, EGU2007-A-07368.
op_relation Timmermann, R. , Böning, C. , Schröter, J. orcid:0000-0002-9240-5798 and Danilov, S. orcid:0000-0001-8098-182X (2007) On the representation of the Southern Ocean in a finite-element coupled sea ice-ocean model , Geophysical Research Abstracts 9, EGU2007-A-07368. . hdl:10013/epic.27926
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