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dc.contributor.authorKnutson, Thomas
dc.contributor.authorCamargo, Suzana J.
dc.contributor.authorChan, Johnny C. L.
dc.contributor.authorEmanuel, Kerry Andrew
dc.contributor.authorHo, Chang-Hoi
dc.contributor.authorKossin, James
dc.contributor.authorMohapatra, Mrutyunjay
dc.contributor.authorSatoh, Masaki
dc.contributor.authorSugi, Masato
dc.contributor.authorWalsh, Kevin
dc.contributor.authorWu, Liguang
dc.date.accessioned2020-05-29T14:53:33Z
dc.date.available2020-05-29T14:53:33Z
dc.date.issued2019-10
dc.identifier.issn0003-0007
dc.identifier.issn1520-0477
dc.identifier.urihttps://hdl.handle.net/1721.1/125577
dc.description.abstractAn assessment was made of whether detectable changes in tropical cyclone (TC) activity are identifiable in observations and whether any changes can be attributed to anthropogenic climate change. Overall, historical data suggest detectable TC activity changes in some regions associated with TC track changes, while data quality and quantity issues create greater challenges for analyses based on TC intensity and frequency. A number of specific published conclusions (case studies) about possible detectable anthropogenic influence on TCs were assessed using the conventional approach of preferentially avoiding type I errors (i.e., overstating anthropogenic influence or detection). We conclude there is at least low to medium confidence that the observed poleward migration of the latitude of maximum intensity in the western North Pacific is detectable, or highly unusual compared to expected natural variability. Opinion on the author team was divided on whether any observed TC changes demonstrate discernible anthropogenic influence, or whether any other observed changes represent detectable changes. The issue was then reframed by assessing evidence for detectable anthropogenic influence while seeking to reduce the chance of type II errors (i.e., missing or understating anthropogenic influence or detection). For this purpose, we used a much weaker “balance of evidence” criterion for assessment. This leads to a number of more speculative TC detection and/or attribution statements, which we recognize have substantial potential for being false alarms (i.e., overstating anthropogenic influence or detection) but which may be useful for risk assessment. Several examples of these alternative statements, derived using this approach, are presented in the report.en_US
dc.language.isoen
dc.publisherAmerican Meteorological Societyen_US
dc.relation.isversionofhttp://dx.doi.org/10.1175/bams-d-18-0189.1en_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.titleTropical Cyclones and Climate Change Assessment: Part I: Detection and Attributionen_US
dc.typeArticleen_US
dc.identifier.citationKnutson, Thomas et al. "Tropical Cyclones and Climate Change Assessment: Part I: Detection and Attribution." Bulletin of the American Meteorological Society 100, 10 (October 2019): 1987-2008 © 2019 American Meteorological Societyen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.relation.journalBulletin of the American Meteorological Societyen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2020-01-15T14:59:53Z
dspace.date.submission2020-01-15T14:59:55Z
mit.journal.volume100en_US
mit.journal.issue10en_US
mit.metadata.statusComplete


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