Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8722
DC FieldValueLanguage
dc.contributor.authorallScoccimarro, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallGualdi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallZampieri, M.; CMCCen
dc.contributor.authorallBellucci, A.; CMCCen
dc.contributor.authorallNavarra, A.; CMCCen
dc.date.accessioned2013-06-24T05:57:08Zen
dc.date.available2013-06-24T05:57:08Zen
dc.date.issued2013en
dc.identifier.urihttp://hdl.handle.net/2122/8722en
dc.description.abstractIn this work the authors investigate possible changes in the distribution of heavy precipitation events under a warmer climate, using the results of a set of 20 climate models taking part in the Coupled Model Intercomparison Project phase 5 effort (CMIP5). Future changes are evaluated as the difference between the last four decades of the 21st and the 20th Century assuming the Representative Concentration Pathway RCP8.5 scenario. As a measure of the width of the right tail of the precipitation distribution, we use the difference between the 99th and the 90th percentiles. Despite a slight tendency to underestimate the observed heavy precipitation, the considered CMIP5 models well represent the observed patterns in terms of the ensemble average, during both summer and winter seasons for the 1997-2005 period. Future changes in average precipitation are consistent with previous findings based on CMIP3 models. CMIP5 models show a projected increase for the end of the twenty-first century of the width of the right tail of the precipitation distribution, particularly pronounced over India, South East Asia, Indonesia and Central Africa during boreal summer, as well as over South America and southern Africa during boreal winter.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Meteorological Societyen
dc.relation.ispartofJournal of climateen
dc.relation.ispartofseries20/26 (2013)en
dc.subjectprecipitationen
dc.subjectextreme eventsen
dc.subjectclimate changeen
dc.titleHeavy precipitation events in a warmer climate: results from CMIP5 modelsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber7902–7911en
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.02. Climateen
dc.identifier.doi10.1175/JCLI-D-12-00850.1en
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.issn0894-8755en
dc.relation.eissn1520-0442en
dc.contributor.authorScoccimarro, E.en
dc.contributor.authorGualdi, S.en
dc.contributor.authorZampieri, M.en
dc.contributor.authorBellucci, A.en
dc.contributor.authorNavarra, A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentCMCCen
dc.contributor.departmentCMCCen
dc.contributor.departmentCMCCen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptCMCC-
crisitem.author.deptCMCC-
crisitem.author.deptCMCC, Italy-
crisitem.author.orcid0000-0001-7987-4744-
crisitem.author.orcid0000-0001-7777-8935-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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