A. Chaigneau, Stéphane Law-Chune, A. Melet, A. Voldoire, G. Reffray, L. Aouf
{"title":"Impact of sea level changes on future wave conditions along the coasts of western Europe","authors":"A. Chaigneau, Stéphane Law-Chune, A. Melet, A. Voldoire, G. Reffray, L. Aouf","doi":"10.5194/os-19-1123-2023","DOIUrl":null,"url":null,"abstract":"Abstract. Wind waves and swells are major drivers of coastal environment\nchanges and coastal hazards such as coastal flooding and erosion. Wave\ncharacteristics are sensitive to changes in water depth in shallow and\nintermediate waters. However, wave models used for historical simulations\nand projections typically do not account for sea level changes whether from\ntides, storm surges, or long-term sea level rise. In this study, the\nsensitivity of projected changes in wave characteristics to the sea level changes is investigated along the Atlantic\nEuropean coastline. For this purpose, a global wave model is dynamically\ndownscaled over the northeastern Atlantic for the 1970–2100 period under the\nSSP5–8.5 climate change scenario. Twin experiments are performed with or\nwithout the inclusion of hourly sea level variations from regional 3D ocean\nsimulations in the regional wave model. The largest impact of sea level changes on waves is located on the wide continental shelf\nwhere shallow-water dynamics prevail, especially in macro-tidal areas. For\ninstance, in the Bay of Mont-Saint-Michel in France, due to an average tidal range of\n10 m, extreme historical wave heights were found to be up to 1 m\nhigher (+30 %) when sea level variations are included. At the end of\nthe 21st century, extreme significant wave heights are larger by up to\n+40 % (+60 cm), mainly due to the effect of tides and mean sea level\nrise. The estimates provided in this study only partially represent the\nprocesses responsible for the sea-level–wave non-linear interactions due to\nmodel limitations in terms of resolution and the processes included.\n","PeriodicalId":19535,"journal":{"name":"Ocean Science","volume":"10 1","pages":""},"PeriodicalIF":4.1000,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ocean Science","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/os-19-1123-2023","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Abstract. Wind waves and swells are major drivers of coastal environment
changes and coastal hazards such as coastal flooding and erosion. Wave
characteristics are sensitive to changes in water depth in shallow and
intermediate waters. However, wave models used for historical simulations
and projections typically do not account for sea level changes whether from
tides, storm surges, or long-term sea level rise. In this study, the
sensitivity of projected changes in wave characteristics to the sea level changes is investigated along the Atlantic
European coastline. For this purpose, a global wave model is dynamically
downscaled over the northeastern Atlantic for the 1970–2100 period under the
SSP5–8.5 climate change scenario. Twin experiments are performed with or
without the inclusion of hourly sea level variations from regional 3D ocean
simulations in the regional wave model. The largest impact of sea level changes on waves is located on the wide continental shelf
where shallow-water dynamics prevail, especially in macro-tidal areas. For
instance, in the Bay of Mont-Saint-Michel in France, due to an average tidal range of
10 m, extreme historical wave heights were found to be up to 1 m
higher (+30 %) when sea level variations are included. At the end of
the 21st century, extreme significant wave heights are larger by up to
+40 % (+60 cm), mainly due to the effect of tides and mean sea level
rise. The estimates provided in this study only partially represent the
processes responsible for the sea-level–wave non-linear interactions due to
model limitations in terms of resolution and the processes included.
期刊介绍:
Ocean Science (OS) is a not-for-profit international open-access scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of ocean science: experimental, theoretical, and laboratory. The primary objective is to publish a very high-quality scientific journal with free Internet-based access for researchers and other interested people throughout the world.
Electronic submission of articles is used to keep publication costs to a minimum. The costs will be covered by a moderate per-page charge paid by the authors. The peer-review process also makes use of the Internet. It includes an 8-week online discussion period with the original submitted manuscript and all comments. If accepted, the final revised paper will be published online.
Ocean Science covers the following fields: ocean physics (i.e. ocean structure, circulation, tides, and internal waves); ocean chemistry; biological oceanography; air–sea interactions; ocean models – physical, chemical, biological, and biochemical; coastal and shelf edge processes; paleooceanography.