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  The Earth system model CLIMBER-X v1.0 - Part 1: Climate model description and validation

Willeit, M., Ganopolski, A., Robinson, A., Edwards, N. R. (2022): The Earth system model CLIMBER-X v1.0 - Part 1: Climate model description and validation. - Geoscientific Model Development, 15, 14, 5905-5948.
https://doi.org/10.5194/gmd-15-5905-2022

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 ???ViewItemFull_lblCreators???:
Willeit, Matteo1, ???ENUM_CREATORROLE_AUTHOR???           
Ganopolski, Andrey1, ???ENUM_CREATORROLE_AUTHOR???           
Robinson, Alexander1, ???ENUM_CREATORROLE_AUTHOR???           
Edwards, Neil R.2, ???ENUM_CREATORROLE_AUTHOR???
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1Potsdam Institute for Climate Impact Research, ou_persistent13              
2External Organizations, ou_persistent22              

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 ???ViewItemFull_lblAbstract???: The newly developed fast Earth system model CLIMBER-X is presented. The climate component of CLIMBER-X consists of a 2.5D semi-empirical statistical-dynamical atmosphere model, a 3D frictional-geostrophic ocean model, a dynamic-thermodynamic sea ice model and a land surface model. All model components are discretized on a regular lat-lon grid with a horizontal resolution of 5° × 5°. The model has a throughput of ~10,000 simulation years per day on a single node with 16 CPUs on a high performance computer and is designed to simulate the evolution of the Earth system on temporal scales ranging from decades to > 100,000 years. A comprehensive evaluation of the model performance for present day and the historical period shows that CLIMBER-X is capable of realistically reproducing many observed climate characteristics, with results that generally lie within the range of state-of-the-art general circulation models. The analysis of model performance is complemented by a thorough assessment of climate feedbacks and model sensitivities to changes in external forcings and boundary conditions. CLIMBER-X also includes a detailed representation of the global carbon cycle and is coupled to an ice sheet model, which will be described in separate papers. CLIMBER-X is available as open--source code and is expected to be a useful tool for studying past climate changes and for the investigation of the long-term future evolution of the climate.

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???ViewItemFull_lblLanguages???: eng - English
 ???ViewItemFull_lblDates???: 2022-07-202022-07-282022-07-28
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 ???ViewItemFull_lblPages???: 44
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 ???ViewItemFull_lblIdentifiers???: ???ENUM_IDENTIFIERTYPE_PIKDOMAIN???: RD1 - Earth System Analysis
???ENUM_IDENTIFIERTYPE_ORGANISATIONALK???: RD1 - Earth System Analysis
???ENUM_IDENTIFIERTYPE_WORKINGGROUP???: Long-Term Dynamics of the Earth System
???ENUM_IDENTIFIERTYPE_MODELMETHOD???: CLIMBER
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Atmosphere
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Oceans
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Paleoclimate
???ENUM_IDENTIFIERTYPE_MDB_ID???: pending
???ENUM_IDENTIFIERTYPE_OATYPE???: Gold Open Access
???ENUM_IDENTIFIERTYPE_DOI???: 10.5194/gmd-15-5905-2022
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???ViewItemFull_lblSourceTitle???: Geoscientific Model Development
???ViewItemFull_lblSourceGenre???: ???ENUM_GENRE_JOURNAL???, SCI, Scopus, p3, oa
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???ENUM_IDENTIFIERTYPE_PUBLISHER???: Copernicus