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Edited by Anny Cazenave, Centre National d'Etudes Spatiales, Toulouse, France, and approved July 26, 2016 (received for review March 16, 2016)
Significance
This study demonstrates quantitatively that the frequency of Hurricane Sandy-like extreme flood events has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century, due to the compound effects of sea level rise and storm climatology change.
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.
Footnotes
- ↵1To whom correspondence should be addressed. Email: nlin{at}princeton.edu.
Author contributions: N.L., B.P.H., and J.P.D. designed research; N.L. and R.E.K. performed research; N.L. analyzed data; and N.L., R.E.K., B.P.H., and J.P.D. wrote the paper.
The authors declare no conflict of interest.
This article is a PNAS Direct Submission.
Data deposition: The data reported in this paper have been deposited at arks.princeton.edu/ark:/88435/dsp01fn107142z.
Freely available online through the PNAS open access option.
Sandy's flood frequency from 1800 to 2100
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