Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean
Over recent decades, the Arctic Ocean has experienced dramatic variations due to climate change. By retreating at a rate of 13% per decade, sea ice has opened up significant areas of ocean, enabling wind to blow over larger fetches and potentially enhancing wave climate. Considering the intense seas...
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ftdoajarticles:oai:doaj.org/article:bc1b808d01b24087ae6c064122fba686 2023-05-15T14:48:11+02:00 Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean Isabela S. Cabral Ian R. Young Alessandro Toffoli 2022-05-01T00:00:00Z https://doi.org/10.3389/fmars.2022.802022 https://doaj.org/article/bc1b808d01b24087ae6c064122fba686 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2022.802022/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2022.802022 https://doaj.org/article/bc1b808d01b24087ae6c064122fba686 Frontiers in Marine Science, Vol 9 (2022) wind extremes wave extremes Arctic Ocean climate change non-stationary statistics Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2022 ftdoajarticles https://doi.org/10.3389/fmars.2022.802022 2022-12-30T23:51:20Z Over recent decades, the Arctic Ocean has experienced dramatic variations due to climate change. By retreating at a rate of 13% per decade, sea ice has opened up significant areas of ocean, enabling wind to blow over larger fetches and potentially enhancing wave climate. Considering the intense seasonality and the rapid changes to the Arctic Ocean, a non-stationary approach is applied to time-varying statistical properties to investigate historical trends of extreme values. The analysis is based on a 28-year wave hindcast (from 1991 to 2018) that was simulated using the WAVEWATCH III wave model forced by ERA5 winds. Despite a marginal increase in wind speed (up to about 5%), results demonstrate substantial seasonal differences and robust positive trends in extreme wave height, especially in the Beaufort and East Siberian seas, with increasing rates in areal average of the 100-year return period up to 60%. The reported variations in extreme wave height are directly associated with a more effective wind forcing in emerging open waters that drives waves to build up more energy, thus confirming the positive feedback of sea ice decline on wave climate. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Frontiers in Marine Science 9 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
wind extremes wave extremes Arctic Ocean climate change non-stationary statistics Science Q General. Including nature conservation geographical distribution QH1-199.5 |
spellingShingle |
wind extremes wave extremes Arctic Ocean climate change non-stationary statistics Science Q General. Including nature conservation geographical distribution QH1-199.5 Isabela S. Cabral Ian R. Young Alessandro Toffoli Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
topic_facet |
wind extremes wave extremes Arctic Ocean climate change non-stationary statistics Science Q General. Including nature conservation geographical distribution QH1-199.5 |
description |
Over recent decades, the Arctic Ocean has experienced dramatic variations due to climate change. By retreating at a rate of 13% per decade, sea ice has opened up significant areas of ocean, enabling wind to blow over larger fetches and potentially enhancing wave climate. Considering the intense seasonality and the rapid changes to the Arctic Ocean, a non-stationary approach is applied to time-varying statistical properties to investigate historical trends of extreme values. The analysis is based on a 28-year wave hindcast (from 1991 to 2018) that was simulated using the WAVEWATCH III wave model forced by ERA5 winds. Despite a marginal increase in wind speed (up to about 5%), results demonstrate substantial seasonal differences and robust positive trends in extreme wave height, especially in the Beaufort and East Siberian seas, with increasing rates in areal average of the 100-year return period up to 60%. The reported variations in extreme wave height are directly associated with a more effective wind forcing in emerging open waters that drives waves to build up more energy, thus confirming the positive feedback of sea ice decline on wave climate. |
format |
Article in Journal/Newspaper |
author |
Isabela S. Cabral Ian R. Young Alessandro Toffoli |
author_facet |
Isabela S. Cabral Ian R. Young Alessandro Toffoli |
author_sort |
Isabela S. Cabral |
title |
Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
title_short |
Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
title_full |
Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
title_fullStr |
Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
title_full_unstemmed |
Long-Term and Seasonal Variability of Wind and Wave Extremes in the Arctic Ocean |
title_sort |
long-term and seasonal variability of wind and wave extremes in the arctic ocean |
publisher |
Frontiers Media S.A. |
publishDate |
2022 |
url |
https://doi.org/10.3389/fmars.2022.802022 https://doaj.org/article/bc1b808d01b24087ae6c064122fba686 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Climate change Sea ice |
genre_facet |
Arctic Arctic Ocean Climate change Sea ice |
op_source |
Frontiers in Marine Science, Vol 9 (2022) |
op_relation |
https://www.frontiersin.org/articles/10.3389/fmars.2022.802022/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2022.802022 https://doaj.org/article/bc1b808d01b24087ae6c064122fba686 |
op_doi |
https://doi.org/10.3389/fmars.2022.802022 |
container_title |
Frontiers in Marine Science |
container_volume |
9 |
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1766319284260175872 |