Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era

In a changing climate, future inundation of the United States’ Atlantic coast will depend on both storm surges during tropical cyclones and the rising relative sea levels on which those surges occur. However, the observational record of tropical cyclones in the North Atlantic basin is too short (A.D...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Reed, Andra J., Mann, Michael E., Lin, Ning, Horton, Benjamin P., Kemp, Andrew C., Donnelly, Jeffrey P., Emanuel, Kerry Andrew
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate
Format: Article in Journal/Newspaper
Language:English
Published: National Academy of Sciences (U.S.) 2015
Subjects:
Online Access:http://hdl.handle.net/1721.1/102265
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spelling ftmit:oai:dspace.mit.edu:1721.1/102265 2023-06-11T04:14:34+02:00 Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era Reed, Andra J. Mann, Michael E. Lin, Ning Horton, Benjamin P. Kemp, Andrew C. Donnelly, Jeffrey P. Emanuel, Kerry Andrew Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate Emanuel, Kerry Andrew 2015-07 application/pdf http://hdl.handle.net/1721.1/102265 en_US eng National Academy of Sciences (U.S.) http://dx.doi.org/10.1073/pnas.1513127112 Proceedings of the National Academy of Sciences 0027-8424 1091-6490 http://hdl.handle.net/1721.1/102265 Reed, Andra J., Michael E. Mann, Kerry A. Emanuel, Ning Lin, Benjamin P. Horton, Andrew C. Kemp, and Jeffrey P. Donnelly. “Increased Threat of Tropical Cyclones and Coastal Flooding to New York City During the Anthropogenic Era.” Proc Natl Acad Sci USA 112, no. 41 (September 28, 2015): 12610–12615. orcid:0000-0002-2066-2082 Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. National Academy of Sciences (U.S.) Article http://purl.org/eprint/type/JournalArticle 2015 ftmit https://doi.org/10.1073/pnas.1513127112 2023-05-29T07:30:33Z In a changing climate, future inundation of the United States’ Atlantic coast will depend on both storm surges during tropical cyclones and the rising relative sea levels on which those surges occur. However, the observational record of tropical cyclones in the North Atlantic basin is too short (A.D. 1851 to present) to accurately assess long-term trends in storm activity. To overcome this limitation, we use proxy sea level records, and downscale three CMIP5 models to generate large synthetic tropical cyclone data sets for the North Atlantic basin; driving climate conditions span from A.D. 850 to A.D. 2005. We compare pre-anthropogenic era (A.D. 850–1800) and anthropogenic era (A.D.1970–2005) storm surge model results for New York City, exposing links between increased rates of sea level rise and storm flood heights. We find that mean flood heights increased by ∼1.24 m (due mainly to sea level rise) from ∼A.D. 850 to the anthropogenic era, a result that is significant at the 99% confidence level. Additionally, changes in tropical cyclone characteristics have led to increases in the extremes of the types of storms that create the largest storm surges for New York City. As a result, flood risk has greatly increased for the region; for example, the 500-y return period for a ∼2.25-m flood height during the pre-anthropogenic era has decreased to ∼24.4 y in the anthropogenic era. Our results indicate the impacts of climate change on coastal inundation, and call for advanced risk management strategies. National Oceanic and Atmospheric Administration (Grant 424-18 45GZ) National Oceanic and Atmospheric Administration (Grant NA11OAR4310101) National Science Foundation (U.S.) (Award OCE 1458904) Article in Journal/Newspaper North Atlantic DSpace@MIT (Massachusetts Institute of Technology) Proceedings of the National Academy of Sciences 112 41 12610 12615
institution Open Polar
collection DSpace@MIT (Massachusetts Institute of Technology)
op_collection_id ftmit
language English
description In a changing climate, future inundation of the United States’ Atlantic coast will depend on both storm surges during tropical cyclones and the rising relative sea levels on which those surges occur. However, the observational record of tropical cyclones in the North Atlantic basin is too short (A.D. 1851 to present) to accurately assess long-term trends in storm activity. To overcome this limitation, we use proxy sea level records, and downscale three CMIP5 models to generate large synthetic tropical cyclone data sets for the North Atlantic basin; driving climate conditions span from A.D. 850 to A.D. 2005. We compare pre-anthropogenic era (A.D. 850–1800) and anthropogenic era (A.D.1970–2005) storm surge model results for New York City, exposing links between increased rates of sea level rise and storm flood heights. We find that mean flood heights increased by ∼1.24 m (due mainly to sea level rise) from ∼A.D. 850 to the anthropogenic era, a result that is significant at the 99% confidence level. Additionally, changes in tropical cyclone characteristics have led to increases in the extremes of the types of storms that create the largest storm surges for New York City. As a result, flood risk has greatly increased for the region; for example, the 500-y return period for a ∼2.25-m flood height during the pre-anthropogenic era has decreased to ∼24.4 y in the anthropogenic era. Our results indicate the impacts of climate change on coastal inundation, and call for advanced risk management strategies. National Oceanic and Atmospheric Administration (Grant 424-18 45GZ) National Oceanic and Atmospheric Administration (Grant NA11OAR4310101) National Science Foundation (U.S.) (Award OCE 1458904)
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate
Emanuel, Kerry Andrew
format Article in Journal/Newspaper
author Reed, Andra J.
Mann, Michael E.
Lin, Ning
Horton, Benjamin P.
Kemp, Andrew C.
Donnelly, Jeffrey P.
Emanuel, Kerry Andrew
spellingShingle Reed, Andra J.
Mann, Michael E.
Lin, Ning
Horton, Benjamin P.
Kemp, Andrew C.
Donnelly, Jeffrey P.
Emanuel, Kerry Andrew
Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
author_facet Reed, Andra J.
Mann, Michael E.
Lin, Ning
Horton, Benjamin P.
Kemp, Andrew C.
Donnelly, Jeffrey P.
Emanuel, Kerry Andrew
author_sort Reed, Andra J.
title Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
title_short Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
title_full Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
title_fullStr Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
title_full_unstemmed Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era
title_sort increased threat of tropical cyclones and coastal flooding to new york city during the anthropogenic era
publisher National Academy of Sciences (U.S.)
publishDate 2015
url http://hdl.handle.net/1721.1/102265
genre North Atlantic
genre_facet North Atlantic
op_source National Academy of Sciences (U.S.)
op_relation http://dx.doi.org/10.1073/pnas.1513127112
Proceedings of the National Academy of Sciences
0027-8424
1091-6490
http://hdl.handle.net/1721.1/102265
Reed, Andra J., Michael E. Mann, Kerry A. Emanuel, Ning Lin, Benjamin P. Horton, Andrew C. Kemp, and Jeffrey P. Donnelly. “Increased Threat of Tropical Cyclones and Coastal Flooding to New York City During the Anthropogenic Era.” Proc Natl Acad Sci USA 112, no. 41 (September 28, 2015): 12610–12615.
orcid:0000-0002-2066-2082
op_rights Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
op_doi https://doi.org/10.1073/pnas.1513127112
container_title Proceedings of the National Academy of Sciences
container_volume 112
container_issue 41
container_start_page 12610
op_container_end_page 12615
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