Projected 21st century changes in extreme wind-wave events

We describe an innovative approach to estimate global changes in extreme wave conditions by 2100, as a result of projected climate change. We generate a synthetic dataset from an ensemble of wave models forced by independent climate simulation winds, enhancing statistical confidence associated with...

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Published in:Science Advances
Main Authors: Meucci, Alberto, Young, Ian R., Hemer, Mark, Kirezci, Ebru, Ranasinghe, Roshanka
Format: Text
Language:English
Published: American Association for the Advancement of Science 2020
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7286683/
http://www.ncbi.nlm.nih.gov/pubmed/32577512
https://doi.org/10.1126/sciadv.aaz7295
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author Meucci, Alberto
Young, Ian R.
Hemer, Mark
Kirezci, Ebru
Ranasinghe, Roshanka
author_facet Meucci, Alberto
Young, Ian R.
Hemer, Mark
Kirezci, Ebru
Ranasinghe, Roshanka
author_sort Meucci, Alberto
collection PubMed Central (PMC)
container_issue 24
container_start_page eaaz7295
container_title Science Advances
container_volume 6
description We describe an innovative approach to estimate global changes in extreme wave conditions by 2100, as a result of projected climate change. We generate a synthetic dataset from an ensemble of wave models forced by independent climate simulation winds, enhancing statistical confidence associated with projected changes in extreme wave conditions. Under two IPCC representative greenhouse gas emission scenarios (RCP4.5 and RCP8.5), we find that the magnitude of a 1 in 100-year significant wave height (H(s)) event increases by 5 to 15% over the Southern Ocean by the end of the 21st century, compared to the 1979–2005 period. The North Atlantic shows a decrease at low to mid latitudes (≈5 to 15%) and an increase at high latitudes (≈10%). The extreme significant wave height in the North Pacific increases at high latitudes by 5 to 10%. The ensemble approach used here allows statistical confidence in projected changes of extremes.
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genre North Atlantic
Southern Ocean
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geographic Southern Ocean
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op_doi https://doi.org/10.1126/sciadv.aaz7295
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7286683/
http://www.ncbi.nlm.nih.gov/pubmed/32577512
http://dx.doi.org/10.1126/sciadv.aaz7295
op_rights Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).
http://creativecommons.org/licenses/by-nc/4.0/
This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial license (http://creativecommons.org/licenses/by-nc/4.0/) , which permits use, distribution, and reproduction in any medium, so long as the resultant use is not for commercial advantage and provided the original work is properly cited.
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spelling ftpubmed:oai:pubmedcentral.nih.gov:7286683 2025-01-16T23:38:59+00:00 Projected 21st century changes in extreme wind-wave events Meucci, Alberto Young, Ian R. Hemer, Mark Kirezci, Ebru Ranasinghe, Roshanka 2020-06-10 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7286683/ http://www.ncbi.nlm.nih.gov/pubmed/32577512 https://doi.org/10.1126/sciadv.aaz7295 en eng American Association for the Advancement of Science http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7286683/ http://www.ncbi.nlm.nih.gov/pubmed/32577512 http://dx.doi.org/10.1126/sciadv.aaz7295 Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). http://creativecommons.org/licenses/by-nc/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial license (http://creativecommons.org/licenses/by-nc/4.0/) , which permits use, distribution, and reproduction in any medium, so long as the resultant use is not for commercial advantage and provided the original work is properly cited. CC-BY-NC Sci Adv Research Articles Text 2020 ftpubmed https://doi.org/10.1126/sciadv.aaz7295 2020-06-28T00:16:14Z We describe an innovative approach to estimate global changes in extreme wave conditions by 2100, as a result of projected climate change. We generate a synthetic dataset from an ensemble of wave models forced by independent climate simulation winds, enhancing statistical confidence associated with projected changes in extreme wave conditions. Under two IPCC representative greenhouse gas emission scenarios (RCP4.5 and RCP8.5), we find that the magnitude of a 1 in 100-year significant wave height (H(s)) event increases by 5 to 15% over the Southern Ocean by the end of the 21st century, compared to the 1979–2005 period. The North Atlantic shows a decrease at low to mid latitudes (≈5 to 15%) and an increase at high latitudes (≈10%). The extreme significant wave height in the North Pacific increases at high latitudes by 5 to 10%. The ensemble approach used here allows statistical confidence in projected changes of extremes. Text North Atlantic Southern Ocean PubMed Central (PMC) Southern Ocean Pacific Science Advances 6 24 eaaz7295
spellingShingle Research Articles
Meucci, Alberto
Young, Ian R.
Hemer, Mark
Kirezci, Ebru
Ranasinghe, Roshanka
Projected 21st century changes in extreme wind-wave events
title Projected 21st century changes in extreme wind-wave events
title_full Projected 21st century changes in extreme wind-wave events
title_fullStr Projected 21st century changes in extreme wind-wave events
title_full_unstemmed Projected 21st century changes in extreme wind-wave events
title_short Projected 21st century changes in extreme wind-wave events
title_sort projected 21st century changes in extreme wind-wave events
topic Research Articles
topic_facet Research Articles
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7286683/
http://www.ncbi.nlm.nih.gov/pubmed/32577512
https://doi.org/10.1126/sciadv.aaz7295