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dc.contributor.authorStratton, RA
dc.contributor.authorSenior, CA
dc.contributor.authorVosper, SB
dc.contributor.authorFolwell, SS
dc.contributor.authorBoutle, IA
dc.contributor.authorEarnshaw, PD
dc.contributor.authorKendon, E
dc.contributor.authorLock, AP
dc.contributor.authorMalcolm, A
dc.contributor.authorManners, J
dc.contributor.authorMorcrette, CJ
dc.contributor.authorShort, C
dc.contributor.authorStirling, AJ
dc.contributor.authorTaylor, CM
dc.contributor.authorTucker, S
dc.contributor.authorWebster, S
dc.contributor.authorWilkinson, JM
dc.date.accessioned2019-11-29T15:32:23Z
dc.date.issued2018-04-02
dc.description.abstractA convection-permitting multiyear regional climate simulation using the Met Office Unified Model has been run for the first time on an Africa-wide domain. The model has been run as part of the Future Climate for Africa (FCFA) Improving Model Processes for African Climate (IMPALA) project, and its configuration, domain, and forcing data are described here in detail. The model [Pan-African Convection-Permitting Regional Climate Simulation with the Met Office UM (CP4-Africa)] uses a 4.5-km horizontal grid spacing at the equator and is run without a convection parameterization, nested within a global atmospheric model driven by observations at the sea surface, which does include a convection scheme. An additional regional simulation, with identical resolution and physical parameterizations to the global model, but with the domain, land surface, and aerosol climatologies of CP4-Africa, has been run to aid in the understanding of the differences between the CP4-Africa and global model, in particular to isolate the impact of the convection parameterization and resolution. The effect of enforcing moisture conservation in CP4-Africa is described and its impact on reducing extreme precipitation values is assessed. Preliminary results from the first five years of the CP4-Africa simulation show substantial improvements in JJA average rainfall compared to the parameterized convection models, with most notably a reduction in the persistent dry bias in West Africa, giving an indication of the benefits to be gained from running a convection-permitting simulation over the whole African continent.en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.identifier.citationVol. 31, pp. 3485 - 3508en_GB
dc.identifier.doi10.1175/JCLI-D-17-0503.1
dc.identifier.grantnumberNE/M017214/1en_GB
dc.identifier.grantnumberNE/M017230/1en_GB
dc.identifier.urihttp://hdl.handle.net/10871/39883
dc.language.isoenen_GB
dc.publisherAmerican Meteorological Societyen_GB
dc.rights© 2018 American Meteorological Society. Open accessen_GB
dc.subjectAtmosphereen_GB
dc.subjectAfricaen_GB
dc.subjectConvectionen_GB
dc.subjectClimate modelsen_GB
dc.subjectRegional modelsen_GB
dc.titleA Pan-African Convection-Permitting Regional Climate Simulation with the Met Office Unified Model: CP4-Africaen_GB
dc.typeArticleen_GB
dc.date.available2019-11-29T15:32:23Z
dc.identifier.issn0894-8755
dc.descriptionThis is the final version. Available on open access from the American Meteorological Society via the DOI in this recorden_GB
dc.identifier.journalJournal of Climateen_GB
rioxxterms.versionVoRen_GB
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2019-11-29T15:28:00Z
refterms.versionFCDVoR
refterms.dateFOA2019-11-29T15:32:25Z
refterms.panelBen_GB
refterms.depositExceptionpublishedGoldOA


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