Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)

The coupled sea-ice ocean model FESOM is based on the finite element method and hydrostatic primitive equa- tions. Both the ocean and ice modules are discretized on the same triangular surface meshes, allowing direct exchange of fluxes and fields between the two components. Recently, this model has...

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Main Authors: Wang, Xuezhu, Wang, Qiang, Sidorenko, Dmitry, Danilov, Sergey, Schröter, Jens, Jung, Thomas
Format: Conference Object
Language:unknown
Published: 2012
Subjects:
Online Access:https://epic.awi.de/id/eprint/30271/
http://meetingorganizer.copernicus.org/EGU2012/EGU2012-427.pdf
https://hdl.handle.net/10013/epic.39520
id ftawi:oai:epic.awi.de:30271
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spelling ftawi:oai:epic.awi.de:30271 2024-09-15T17:51:29+00:00 Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM) Wang, Xuezhu Wang, Qiang Sidorenko, Dmitry Danilov, Sergey Schröter, Jens Jung, Thomas 2012-04-22 https://epic.awi.de/id/eprint/30271/ http://meetingorganizer.copernicus.org/EGU2012/EGU2012-427.pdf https://hdl.handle.net/10013/epic.39520 unknown Wang, X. , Wang, Q. orcid:0000-0002-2704-5394 , Sidorenko, D. orcid:0000-0001-8579-6068 , Danilov, S. orcid:0000-0001-8098-182X , Schröter, J. orcid:0000-0002-9240-5798 and Jung, T. orcid:0000-0002-2651-1293 (2012) Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM) , EGU General Assembly 2012, 22 April 2012 - 27 April 2012 . hdl:10013/epic.39520 EPIC3EGU General Assembly 2012, 2012-04-22-2012-04-27 Conference notRev 2012 ftawi 2024-06-24T04:05:07Z The coupled sea-ice ocean model FESOM is based on the finite element method and hydrostatic primitive equa- tions. Both the ocean and ice modules are discretized on the same triangular surface meshes, allowing direct exchange of fluxes and fields between the two components. Recently, this model has been employed to resolve multi-scale dynamics in the Arctic Ocean. This work is conducted using global simulations with local mesh re- finement in the Arctic Ocean. The global background resolution is 1.5 degree. Two simulations with different resolutions of 24km and 9km in the Arctic region have been conducted. The model performance in the Arctic Ocean is assessed comparing the available observational data. The comparison results demonstrate that the model can well simulate the general ocean circulation and important ocean and sea ice processes, although model param- eters and/or forcing for the focus of the Arctic Ocean modeling need to be further optimized in the future work. The sensitivity of the model performance to local mesh refinement in the Arctic Ocean is analyzed. Conference Object Arctic Arctic Ocean Sea ice 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 The coupled sea-ice ocean model FESOM is based on the finite element method and hydrostatic primitive equa- tions. Both the ocean and ice modules are discretized on the same triangular surface meshes, allowing direct exchange of fluxes and fields between the two components. Recently, this model has been employed to resolve multi-scale dynamics in the Arctic Ocean. This work is conducted using global simulations with local mesh re- finement in the Arctic Ocean. The global background resolution is 1.5 degree. Two simulations with different resolutions of 24km and 9km in the Arctic region have been conducted. The model performance in the Arctic Ocean is assessed comparing the available observational data. The comparison results demonstrate that the model can well simulate the general ocean circulation and important ocean and sea ice processes, although model param- eters and/or forcing for the focus of the Arctic Ocean modeling need to be further optimized in the future work. The sensitivity of the model performance to local mesh refinement in the Arctic Ocean is analyzed.
format Conference Object
author Wang, Xuezhu
Wang, Qiang
Sidorenko, Dmitry
Danilov, Sergey
Schröter, Jens
Jung, Thomas
spellingShingle Wang, Xuezhu
Wang, Qiang
Sidorenko, Dmitry
Danilov, Sergey
Schröter, Jens
Jung, Thomas
Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
author_facet Wang, Xuezhu
Wang, Qiang
Sidorenko, Dmitry
Danilov, Sergey
Schröter, Jens
Jung, Thomas
author_sort Wang, Xuezhu
title Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
title_short Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
title_full Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
title_fullStr Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
title_full_unstemmed Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM)
title_sort assessment of an arctic ocean model in a global configuration using the finite element sea-ice ocean model (fesom)
publishDate 2012
url https://epic.awi.de/id/eprint/30271/
http://meetingorganizer.copernicus.org/EGU2012/EGU2012-427.pdf
https://hdl.handle.net/10013/epic.39520
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source EPIC3EGU General Assembly 2012, 2012-04-22-2012-04-27
op_relation Wang, X. , Wang, Q. orcid:0000-0002-2704-5394 , Sidorenko, D. orcid:0000-0001-8579-6068 , Danilov, S. orcid:0000-0001-8098-182X , Schröter, J. orcid:0000-0002-9240-5798 and Jung, T. orcid:0000-0002-2651-1293 (2012) Assessment of an Arctic Ocean model in a global configuration using the Finite Element Sea-ice Ocean Model (FESOM) , EGU General Assembly 2012, 22 April 2012 - 27 April 2012 . hdl:10013/epic.39520
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