300 year simulation with the coupled FESOM/ECHAM5 model

We present a global climate model setup where the Finite-Element Sea-Ice Ocean Model (FESOM) has been coupled to the atmospheric model ECHAM5. The major difference of this setup to other climate models is the ocean component which supports variable resolution. The latter allows to refine the areas o...

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Main Authors: Sidorenko, Dmitry, Rackow, Thomas, Semmler, T., Jung, Thomas, Wang, Qiang, Danilov, Sergey, Schröter, Jens
Format: Conference Object
Language:unknown
Published: 2012
Subjects:
Online Access:https://epic.awi.de/id/eprint/30743/
https://hdl.handle.net/10013/epic.39666
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spelling ftawi:oai:epic.awi.de:30743 2024-09-15T18:35:27+00:00 300 year simulation with the coupled FESOM/ECHAM5 model Sidorenko, Dmitry Rackow, Thomas Semmler, T. Jung, Thomas Wang, Qiang Danilov, Sergey Schröter, Jens 2012-04-23 https://epic.awi.de/id/eprint/30743/ https://hdl.handle.net/10013/epic.39666 unknown Sidorenko, D. orcid:0000-0001-8579-6068 , Rackow, T. orcid:0000-0002-5468-575X , Semmler, T. orcid:0000-0002-2254-4901 , Jung, T. orcid:0000-0002-2651-1293 , Wang, Q. orcid:0000-0002-2704-5394 , Danilov, S. orcid:0000-0001-8098-182X and Schröter, J. orcid:0000-0002-9240-5798 (2012) 300 year simulation with the coupled FESOM/ECHAM5 model , EGU General Assembly, Vienna, Austria, 22 April 2012 - 27 April 2012 . hdl:10013/epic.39666 EPIC3EGU General Assembly, Vienna, Austria, 2012-04-22-2012-04-27 Conference notRev 2012 ftawi 2024-06-24T04:05:07Z We present a global climate model setup where the Finite-Element Sea-Ice Ocean Model (FESOM) has been coupled to the atmospheric model ECHAM5. The major difference of this setup to other climate models is the ocean component which supports variable resolution. The latter allows to refine the areas of particular interest in the global context and to resolve narrow straits where it is needed. Current model setup has a resolution varying from 30 to 200 km in the ocean and T63L31 (~1.8°) configuration in the atmosphere. We present 300 year integration results, discuss model variability and trends. It is shown that the climate state simulated by FESOM/ECHAM is in most cases within the spread of other models. On another hand we address the technical complexity of this setup, linked to an exchange between unstructured and structured meshes. These have different geometry, representation of coastlines and different rules for the flux definition. This implies that additional strategies have to be developed in order to preserve the flux conservation. We summarize the problems and suggest our compromised solutions. Conference Object 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 We present a global climate model setup where the Finite-Element Sea-Ice Ocean Model (FESOM) has been coupled to the atmospheric model ECHAM5. The major difference of this setup to other climate models is the ocean component which supports variable resolution. The latter allows to refine the areas of particular interest in the global context and to resolve narrow straits where it is needed. Current model setup has a resolution varying from 30 to 200 km in the ocean and T63L31 (~1.8°) configuration in the atmosphere. We present 300 year integration results, discuss model variability and trends. It is shown that the climate state simulated by FESOM/ECHAM is in most cases within the spread of other models. On another hand we address the technical complexity of this setup, linked to an exchange between unstructured and structured meshes. These have different geometry, representation of coastlines and different rules for the flux definition. This implies that additional strategies have to be developed in order to preserve the flux conservation. We summarize the problems and suggest our compromised solutions.
format Conference Object
author Sidorenko, Dmitry
Rackow, Thomas
Semmler, T.
Jung, Thomas
Wang, Qiang
Danilov, Sergey
Schröter, Jens
spellingShingle Sidorenko, Dmitry
Rackow, Thomas
Semmler, T.
Jung, Thomas
Wang, Qiang
Danilov, Sergey
Schröter, Jens
300 year simulation with the coupled FESOM/ECHAM5 model
author_facet Sidorenko, Dmitry
Rackow, Thomas
Semmler, T.
Jung, Thomas
Wang, Qiang
Danilov, Sergey
Schröter, Jens
author_sort Sidorenko, Dmitry
title 300 year simulation with the coupled FESOM/ECHAM5 model
title_short 300 year simulation with the coupled FESOM/ECHAM5 model
title_full 300 year simulation with the coupled FESOM/ECHAM5 model
title_fullStr 300 year simulation with the coupled FESOM/ECHAM5 model
title_full_unstemmed 300 year simulation with the coupled FESOM/ECHAM5 model
title_sort 300 year simulation with the coupled fesom/echam5 model
publishDate 2012
url https://epic.awi.de/id/eprint/30743/
https://hdl.handle.net/10013/epic.39666
genre Sea ice
genre_facet Sea ice
op_source EPIC3EGU General Assembly, Vienna, Austria, 2012-04-22-2012-04-27
op_relation Sidorenko, D. orcid:0000-0001-8579-6068 , Rackow, T. orcid:0000-0002-5468-575X , Semmler, T. orcid:0000-0002-2254-4901 , Jung, T. orcid:0000-0002-2651-1293 , Wang, Q. orcid:0000-0002-2704-5394 , Danilov, S. orcid:0000-0001-8098-182X and Schröter, J. orcid:0000-0002-9240-5798 (2012) 300 year simulation with the coupled FESOM/ECHAM5 model , EGU General Assembly, Vienna, Austria, 22 April 2012 - 27 April 2012 . hdl:10013/epic.39666
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