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dc.contributor.authorDonnelly, Jeffrey P.  Concept link
dc.contributor.authorHawkes, Andrea D.  Concept link
dc.contributor.authorLane, D. Philip  Concept link
dc.contributor.authorMacDonald, Dana  Concept link
dc.contributor.authorShuman, Bryan N.  Concept link
dc.contributor.authorToomey, Michael R.  Concept link
dc.contributor.authorvan Hengstum, Peter J.  Concept link
dc.contributor.authorWoodruff, Jonathan D.  Concept link
dc.date.accessioned2015-04-14T15:14:08Z
dc.date.available2015-04-14T15:14:08Z
dc.date.issued2015-02-23
dc.identifier.citationEarth's Future 3 (2015): 49–65en_US
dc.identifier.urihttps://hdl.handle.net/1912/7217
dc.description© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Earth's Future 3 (2015): 49–65, doi:10.1002/2014EF000274.en_US
dc.description.abstractHow climate controls hurricane variability has critical implications for society is not well understood. In part, our understanding is hampered by the short and incomplete observational hurricane record. Here we present a synthesis of intense-hurricane activity from the western North Atlantic over the past two millennia, which is supported by a new, exceptionally well-resolved record from Salt Pond, Massachusetts (USA). At Salt Pond, three coarse grained event beds deposited in the historical interval are consistent with severe hurricanes in 1991 (Bob), 1675, and 1635 C.E., and provide modern analogs for 32 other prehistoric event beds. Two intervals of heightened frequency of event bed deposition between 1400 and 1675 C.E. (10 events) and 150 and 1150 C.E. (23 events), represent the local expression of coherent regional patterns in intense-hurricane–induced event beds. Our synthesis indicates that much of the western North Atlantic appears to have been active between 250 and 1150 C.E., with high levels of activity persisting in the Caribbean and Gulf of Mexico until 1400 C.E. This interval was one with relatively warm sea surface temperatures (SSTs) in the main development region (MDR). A shift in activity to the North American east coast occurred ca. 1400 C.E., with more frequent severe hurricane strikes recorded from The Bahamas to New England between 1400 and 1675 C.E. A warm SST anomaly along the western North Atlantic, rather than within the MDR, likely contributed to the later active interval being restricted to the east coast.en_US
dc.description.sponsorshipFunding was provided by US National Science Foundation (awards 0903020 and 1356708), the Risk Prediction Initiative at the Bermuda Institute for Ocean Sciences (BIOS), US Department of Energy National Institute for Climate Change Research, National Oceanic and Atmospheric Administration (award NA11OAR431010), and the Dalio Explore Fund.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherJohn Wiley & Sonsen_US
dc.relation.urihttps://doi.org/10.1002/2014EF000274
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectTropical cyclonesen_US
dc.subjectClimate changeen_US
dc.subjectHoloceneen_US
dc.subjectCommon eraen_US
dc.subjectSea surface temperatureen_US
dc.titleClimate forcing of unprecedented intense-hurricane activity in the last 2000 yearsen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/2014EF000274


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Attribution-NonCommercial-NoDerivatives 4.0 International
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 International