dc.contributor.author | Lin, Ning | |
dc.contributor.author | Emanuel, Kerry Andrew | |
dc.date.accessioned | 2017-06-01T13:37:33Z | |
dc.date.available | 2017-06-01T13:37:33Z | |
dc.date.issued | 2015-08 | |
dc.date.submitted | 2015-03 | |
dc.identifier.issn | 1758-678X | |
dc.identifier.issn | 1758-6798 | |
dc.identifier.uri | http://hdl.handle.net/1721.1/109495 | |
dc.description.abstract | We define ‘grey swan’ tropical cyclones as high-impact storms that would not be predicted based on history but may be foreseeable using physical knowledge together with historical data. Here we apply a climatological–hydrodynamic method to estimate grey swan tropical cyclone storm surge threat for three highly vulnerable coastal regions. We identify a potentially large risk in the Persian Gulf, where tropical cyclones have never been recorded, and larger-than-expected threats in Cairns, Australia, and Tampa, Florida. Grey swan tropical cyclones striking Tampa, Cairns and Dubai can generate storm surges of about 6 m, 5.7 m and 4 m, respectively, with estimated annual exceedance probabilities of about 1/10,000. With climate change, these probabilities can increase significantly over the twenty-first century (to 1/3,100–1/1,100 in the middle and 1/2,500–1/700 towards the end of the century for Tampa). Worse grey swan tropical cyclones, inducing surges exceeding 11 m in Tampa and 7 m in Dubai, are also revealed with non-negligible probabilities, especially towards the end of the century. | en_US |
dc.language.iso | en_US | |
dc.publisher | Nature Publishing Group | en_US |
dc.relation.isversionof | http://dx.doi.org/10.1038/nclimate2777 | en_US |
dc.rights | Creative Commons Attribution-Noncommercial-Share Alike | en_US |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-sa/4.0/ | en_US |
dc.source | Prof. Emanuel via Chris Sherratt | en_US |
dc.title | Grey swan tropical cyclones | en_US |
dc.type | Article | en_US |
dc.identifier.citation | Lin, Ning, and Kerry Emanuel. “Grey Swan Tropical Cyclones.” Nature Climate Change 6, no. 1 (August 31, 2015): 106–111. | en_US |
dc.contributor.department | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences | en_US |
dc.contributor.approver | Emanuel, Kerry | en_US |
dc.contributor.mitauthor | Lin, Ning | |
dc.contributor.mitauthor | Emanuel, Kerry Andrew | |
dc.relation.journal | Nature Climate Change | en_US |
dc.eprint.version | Author's final manuscript | en_US |
dc.type.uri | http://purl.org/eprint/type/JournalArticle | en_US |
eprint.status | http://purl.org/eprint/status/PeerReviewed | en_US |
dspace.orderedauthors | Lin, Ning; Emanuel, Kerry | en_US |
dspace.embargo.terms | N | en_US |
dc.identifier.orcid | https://orcid.org/0000-0002-2066-2082 | |
mit.license | PUBLISHER_POLICY | en_US |
mit.metadata.status | Complete | |