{"refrec":{"BRefID":232011,"RR":"<b>Woodruff, J.D.; Irish, L.; Camargo, S.J.</b> (2013). Coastal flooding by tropical cyclones and sea-level rise. <i>Nature (Lond.) 504(7478)</i>: 44-52. <a href=\"http://dx.doi.org/10.1038/nature12855\" target=\"_blank\">http://dx.doi.org/10.1038/nature12855</a>","BEntID":223720,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 504(7478)</i>: 44-52. <a href=\"http://dx.doi.org/10.1038/nature12855\" target=\"_blank\">http://dx.doi.org/10.1038/nature12855</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Woodruff, J.D.; Irish, L.; Camargo, S.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Woodruff, J.D. <i>et al.</i>","Englishabstract":"The future impacts of climate change on landfalling tropical cyclones are unclear. Regardless of this uncertainty, flooding by tropical cyclones will increase as a result of accelerated sea-level rise. Under similar rates of rapid sea-level rise during the early Holocene epoch most low-lying sedimentary coastlines were generally much less resilient to storm impacts. Society must learn to live with a rapidly evolving shoreline that is increasingly prone to flooding from tropical cyclones. 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