Climate Change Contributions to Increasing Compound Flooding Risk in New York City
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bams-BAMS-D-23-0177.1.pdf
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Published version
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Author(s) • • • • • •
Sarhadi, Ali
Rousseau-Rizzi, Raphaël
Mandli, Kyle
Neal, Jeffrey
Wiper, Michael P
Feldmann, Monika
Emanuel, Kerry
Date Issued
February 14, 2024
Journal
Bulletin of the American Meteorological Society
Publisher
American Meteorological Society
Citation
Sarhadi, A., R. Rousseau-Rizzi, K. Mandli, J. Neal, M. P. Wiper, M. Feldmann, and K. Emanuel, 2024: Climate Change Contributions to Increasing Compound Flooding Risk in New York City. Bull. Amer. Meteor. Soc., 105, E337–E356.
Version
Final published version
Abstract
Efforts to meaningfully quantify the changes in coastal compound surge- and rainfall-driven flooding hazard associated with tropical cyclones (TCs) and extratropical cyclones (ETCs) in a warming climate have increased in recent years. Despite substantial progress, however, obtaining actionable details such as the spatially and temporally varying distribution and proximal causes of changing flooding hazard in cities remains a persistent challenge. Here, for the first time, physics-based hydrodynamic flood models driven by rainfall and storm surge simultaneously are used to estimate the magnitude and frequency of compound flooding events. We apply this to the particular case of New York City. We find that sea level rise (SLR) alone will increase the TC and ETC compound flooding hazard more significantly than changes in storm climatology as the climate warms. We also project that the probability of destructive Sandy-like compound flooding will increase by up to 5 times by the end of the century. Our results have strong implications for climate change adaptation in coastal communities.
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DOI of Published Version
https://doi.org/10.1175/bams-d-23-0177.1