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dc.contributor.authorEmanuel, Kerry Andrew
dc.date.accessioned2014-03-24T16:11:05Z
dc.date.available2014-03-24T16:11:05Z
dc.date.issued2013-07
dc.date.submitted2013-01
dc.identifier.issn0027-8424
dc.identifier.issn1091-6490
dc.identifier.urihttp://hdl.handle.net/1721.1/85905
dc.description.abstractA recently developed technique for simulating large [O(10[superscript 4])] numbers of tropical cyclones in climate states described by global gridded data is applied to simulations of historical and future climate states simulated by six Coupled Model Intercomparison Project 5 (CMIP5) global climate models. Tropical cyclones downscaled from the climate of the period 1950–2005 are compared with those of the 21st century in simulations that stipulate that the radiative forcing from greenhouse gases increases by 8.5 W m[superscript -2] over preindustrial values. In contrast to storms that appear explicitly in most global models, the frequency of downscaled tropical cyclones increases during the 21st century in most locations. The intensity of such storms, as measured by their maximum wind speeds, also increases, in agreement with previous results. Increases in tropical cyclone activity are most prominent in the western North Pacific, but are evident in other regions except for the southwestern Pacific. The increased frequency of events is consistent with increases in a genesis potential index based on monthly mean global model output. These results are compared and contrasted with other inferences concerning the effect of global warming on tropical cyclones.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (Grant 0850639)en_US
dc.language.isoen_US
dc.publisherNational Academy of Sciences (U.S.)en_US
dc.relation.isversionofhttp://dx.doi.org/10.1073/pnas.1301293110en_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceNational Academy of Science (U.S.)en_US
dc.titleDownscaling CMIP5 climate models shows increased tropical cyclone activity over the 21st centuryen_US
dc.typeArticleen_US
dc.identifier.citationEmanuel, K. A. “Downscaling CMIP5 Climate Models Shows Increased Tropical Cyclone Activity over the 21st Century.” Proceedings of the National Academy of Sciences 110, no. 30 (July 23, 2013): 12219–12224.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.departmentMassachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climateen_US
dc.contributor.mitauthorEmanuel, Kerry Andrewen_US
dc.relation.journalProceedings of the National Academy of Sciencesen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsEmanuel, K. A.en_US
dc.identifier.orcidhttps://orcid.org/0000-0002-2066-2082
mit.licensePUBLISHER_POLICYen_US
mit.metadata.statusComplete


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