Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/84348
Title: Hurricane Sandy’s flood frequency increasing from year 1800 to 2100
Authors: Lin, Ning
Kopp, Robert E.
Horton, Benjamin P.
Donnelly, Jeffrey P.
Keywords: Storm Surge
Science::Geology
Hurricane Sandy
Issue Date: 2016
Source: Lin, N., Kopp, R. E., Horton, B. P., & Donnelly, J. P. (2016). Hurricane Sandy’s flood frequency increasing from year 1800 to 2100. Proceedings of the National Academy of Sciences, 113(43), 12071-12075. doi:10.1073/pnas.1604386113
Series/Report no.: Proceedings of the National Academy of Sciences
Abstract: Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century. Due to the effect of sea level rise, the return period of Hurricane Sandy’s flood height decreased by a factor of ∼3× from year 1800 to 2000 and is estimated to decrease by a further ∼4.4× from 2000 to 2100 under a moderate-emissions pathway. When potential storm climatology change over the 21st century is also accounted for, Sandy’s return period is estimated to decrease by ∼3× to 17× from 2000 to 2100.
URI: https://hdl.handle.net/10356/84348
http://hdl.handle.net/10220/50421
ISSN: 0027-8424
DOI: http://dx.doi.org/10.1073/pnas.1604386113
Rights: © 2016 The Author(s) (published by National Academy of Sciences). This is an open-access article distributed under the terms of the Creative Commons Attribution License.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:ASE Journal Articles
EOS Journal Articles

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