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Future behavior of wind wave extremes due to climate change

Extreme waves will undergo changes in the future when exposed to different climate change scenarios. These changes are evaluated through the analysis of significant wave height (H(s)) return values and are also compared with annual mean H(s) projections. Hourly time series are analyzed through a sev...

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Autores principales: Lobeto, Hector, Menendez, Melisa, Losada, Iñigo J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8042069/
https://www.ncbi.nlm.nih.gov/pubmed/33846354
http://dx.doi.org/10.1038/s41598-021-86524-4
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author Lobeto, Hector
Menendez, Melisa
Losada, Iñigo J.
author_facet Lobeto, Hector
Menendez, Melisa
Losada, Iñigo J.
author_sort Lobeto, Hector
collection PubMed
description Extreme waves will undergo changes in the future when exposed to different climate change scenarios. These changes are evaluated through the analysis of significant wave height (H(s)) return values and are also compared with annual mean H(s) projections. Hourly time series are analyzed through a seven-member ensemble of wave climate simulations and changes are estimated in H(s) for return periods from 5 to 100 years by the end of the century under RCP4.5 and RCP8.5 scenarios. Despite the underlying uncertainty that characterizes extremes, we obtain robust changes in extreme H(s) over more than approximately 25% of the ocean surface. The results obtained conclude that increases cover wider areas and are larger in magnitude than decreases for higher return periods. The Southern Ocean is the region where the most robust increase in extreme H(s) is projected, showing local increases of over 2 m regardless the analyzed return period under RCP8.5 scenario. On the contrary, the tropical north Pacific shows the most robust decrease in extreme H(s), with local decreases of over 1.5 m. Relevant divergences are found in several ocean regions between the projected behavior of mean and extreme wave conditions. For example, an increase in H(s) return values and a decrease in annual mean H(s) is found in the SE Indian, NW Atlantic and NE Pacific. Therefore, an extrapolation of the expected change in mean wave conditions to extremes in regions presenting such divergences should be adopted with caution, since it may lead to misinterpretation when used for the design of marine structures or in the evaluation of coastal flooding and erosion.
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spelling pubmed-80420692021-04-14 Future behavior of wind wave extremes due to climate change Lobeto, Hector Menendez, Melisa Losada, Iñigo J. Sci Rep Article Extreme waves will undergo changes in the future when exposed to different climate change scenarios. These changes are evaluated through the analysis of significant wave height (H(s)) return values and are also compared with annual mean H(s) projections. Hourly time series are analyzed through a seven-member ensemble of wave climate simulations and changes are estimated in H(s) for return periods from 5 to 100 years by the end of the century under RCP4.5 and RCP8.5 scenarios. Despite the underlying uncertainty that characterizes extremes, we obtain robust changes in extreme H(s) over more than approximately 25% of the ocean surface. The results obtained conclude that increases cover wider areas and are larger in magnitude than decreases for higher return periods. The Southern Ocean is the region where the most robust increase in extreme H(s) is projected, showing local increases of over 2 m regardless the analyzed return period under RCP8.5 scenario. On the contrary, the tropical north Pacific shows the most robust decrease in extreme H(s), with local decreases of over 1.5 m. Relevant divergences are found in several ocean regions between the projected behavior of mean and extreme wave conditions. For example, an increase in H(s) return values and a decrease in annual mean H(s) is found in the SE Indian, NW Atlantic and NE Pacific. Therefore, an extrapolation of the expected change in mean wave conditions to extremes in regions presenting such divergences should be adopted with caution, since it may lead to misinterpretation when used for the design of marine structures or in the evaluation of coastal flooding and erosion. Nature Publishing Group UK 2021-04-12 /pmc/articles/PMC8042069/ /pubmed/33846354 http://dx.doi.org/10.1038/s41598-021-86524-4 Text en © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Lobeto, Hector
Menendez, Melisa
Losada, Iñigo J.
Future behavior of wind wave extremes due to climate change
title Future behavior of wind wave extremes due to climate change
title_full Future behavior of wind wave extremes due to climate change
title_fullStr Future behavior of wind wave extremes due to climate change
title_full_unstemmed Future behavior of wind wave extremes due to climate change
title_short Future behavior of wind wave extremes due to climate change
title_sort future behavior of wind wave extremes due to climate change
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8042069/
https://www.ncbi.nlm.nih.gov/pubmed/33846354
http://dx.doi.org/10.1038/s41598-021-86524-4
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