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dc.contributor.authorPfahl, Stephan
dc.contributor.authorSingh, Martin S.
dc.contributor.authorO'Gorman, Paul
dc.date.accessioned2017-07-07T14:48:38Z
dc.date.available2017-07-07T14:48:38Z
dc.date.issued2015-12
dc.date.submitted2015-07
dc.identifier.issn0894-8755
dc.identifier.issn1520-0442
dc.identifier.urihttp://hdl.handle.net/1721.1/110525
dc.description.abstractCyclones are a key element of extratropical weather and frequently lead to extreme events like wind storms and heavy precipitation. Understanding potential changes of cyclone frequency and intensity is thus essential for a proper assessment of climate change impacts. Here the behavior of extratropical cyclones under strongly varying climate conditions is investigated using idealized climate model simulations in an aquaplanet setup. A cyclone tracking algorithm is applied to assess various statistics of cyclone properties such as intensity, size, lifetime, displacement velocity, and deepening rates. In addition, a composite analysis of intense cyclones is performed. In general, the structure of extratropical cyclones in the idealized simulations is very robust, and changes in major cyclone characteristics are relatively small. Median cyclone intensity, measured in terms of minimum sea level pressure and lower-tropospheric relative vorticity, has a maximum in simulations with global mean temperature slightly warmer than present-day Earth, broadly consistent with the behavior of the eddy kinetic energy analyzed in previous studies. Maximum deepening rates along cyclone tracks behave similarly and are in agreement with linear quasigeostrophic growth rates if the effect of latent heat release on the stratification is taken into account. In contrast to moderate cyclones, the relative vorticity of intense cyclones continues to increase with warming to substantially higher temperatures, and this is associated with enhanced lower-tropospheric potential vorticity anomalies likely caused by increased diabatic heating. Moist processes may, therefore, lead to the further strengthening of intense cyclones in warmer climates even if cyclones weaken on average.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (GS-1148594)en_US
dc.language.isoen_US
dc.publisherAmerican Meteorological Societyen_US
dc.relation.isversionofhttp://dx.doi.org/10.1175/jcli-d-14-00816.1en_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.sourceAmerican Meteorological Societyen_US
dc.titleExtratropical Cyclones in Idealized Simulations of Changed Climatesen_US
dc.typeArticleen_US
dc.identifier.citationPfahl, Stephan; O’Gorman, Paul A. and Singh, Martin S. “Extratropical Cyclones in Idealized Simulations of Changed Climates.” Journal of Climate 28, 23 (December 2015): 9373–9392 © 2015 American Meteorological Societyen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorO'Gorman, Paul
dc.relation.journalJournal of Climateen_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.orderedauthorsPfahl, Stephan; O’Gorman, Paul A.; Singh, Martin S.en_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0003-1748-0816
mit.licensePUBLISHER_POLICYen_US


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