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

dc.contributor.authorWilleit, Matteo
dc.contributor.authorGanopolski, Andrey
dc.contributor.authorRobinson, Alexander James
dc.contributor.authorEdwards, Neil R.
dc.date.accessioned2023-06-22T12:30:18Z
dc.date.available2023-06-22T12:30:18Z
dc.date.issued2022-07-28
dc.description© Author(s) 2022. Matteo Willeit was supported by the German Science Foundation (DFG) grant GA 1202/2-1 and by the BMBF-funded project PalMod. Alexander Robinson was funded by the Ramón y Cajal Programme of the Spanish Ministry for Science, Innovation and Universities (grant no. RYC-2016-20587). We thank the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP5 and CMIP6. We thank the climate modelling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies who support CMIP5, CMIP6 and ESGF. Xavier Fettweiss is thanked for providing the grain size data from simulations of the regional climate model MAR. Data from the RAPID AMOC monitoring project are funded by the Natural Environment Research Council and are freely available from http://www.rapid.ac.uk/rapidmoc (last access: 15 January 2022). This research has been supported by the Bundesministerium für Bildung und Forschung (grant no. PalMod), the Deutsche Forschungsgemeinschaft (grant no. GA 1202/2-1), and the Ministerio de Ciencia e Innovación (grant no. RYC-2016- 20587). The publication of this article was funded by the Open Access Fund of the Leibniz Association.
dc.description.abstractThe newly developed fast Earth system model CLIMBER-X is presented. The climate component of CLIMBER-X consists of a 2.5-D semi-empirical statistical– dynamical atmosphere model, a 3-D frictional–geostrophic ocean model, a dynamic–thermodynamic sea ice model and a land surface model. All the model components are discretized on a regular lat–long 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 the 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-theart 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. Limitations and applicability of the model are critically discussed. 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.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Ciencia e Innovación (MICINN)
dc.description.sponsorshipGerman Science Foundation (DFG)
dc.description.sponsorshipBundesministerium für Bildung und Forschung
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/75707
dc.identifier.doi10.5194/gmd-15-5905-2022
dc.identifier.issn1991-959X
dc.identifier.officialurlhttp://dx.doi.org/10.5194/gmd-15-5905-2022
dc.identifier.relatedurlhttps://gmd.copernicus.org
dc.identifier.urihttps://hdl.handle.net/20.500.14352/72706
dc.issue.number14
dc.journal.titleGeoscientific model development
dc.language.isoeng
dc.page.final5948
dc.page.initial5905
dc.publisherCopernicus Gesellschaft MBH
dc.relation.projectIDRYC-2016-20587
dc.relation.projectIDGA 1202/2-1
dc.relation.projectIDPalMod
dc.rightsAtribución 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/es/
dc.subject.cdu52
dc.subject.keywordMeridional overturning circulation
dc.subject.keywordGlacial maximum experiments
dc.subject.keywordIce-sheet model
dc.subject.keywordLand-use change
dc.subject.keywordIntermediate complexity
dc.subject.keywordSea-ice
dc.subject.keywordThermohaline circulation
dc.subject.keywordOcean-circulation
dc.subject.keywordCoupled model
dc.subject.keywordPart II
dc.subject.ucmFísica atmosférica
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleThe Earth system model CLIMBER-X v1.0-Part 1: climate model description and validation
dc.typejournal article
dc.volume.number15
dspace.entity.typePublication
relation.isAuthorOfPublication0e3eb380-b82c-41bd-9606-afac0ef72d63
relation.isAuthorOfPublication.latestForDiscovery0e3eb380-b82c-41bd-9606-afac0ef72d63

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