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dc.contributor.authorWolf, Tobias
dc.contributor.authorOutten, Stephen
dc.contributor.authorMangini, Fabio
dc.contributor.authorChen, Linling
dc.contributor.authorNilsen, Jan Even Øie
dc.date.accessioned2023-07-03T12:31:57Z
dc.date.available2023-07-03T12:31:57Z
dc.date.created2023-02-28T09:19:36Z
dc.date.issued2023
dc.identifier.issn2296-6463
dc.identifier.urihttps://hdl.handle.net/11250/3075377
dc.description.abstractObserved extreme sea levels are caused by a combination of extreme astronomical tide and extreme storm surge, or by an extreme value in one of these variables and a moderate value in the other. We analyzed measurements from the Norwegian tide gauge network together with storm track data to assess cases of extreme sea level and storm surges. At most stations the highest storm surges only coincided with moderate astronomical tides and vice versa. Simultaneously the extreme storm surges often only coincided with moderate storm intensities. This opens for the possibility of flooding events, where extreme tides and storm surges co-occur, and which could exceed existing sea level records and national building standards. This study also raises the possibility to assess extreme sea level return values as a three-variable system, treating separately the astronomical tide, storm location and storm intensity, instead of the one- or two-variable approach currently used.en_US
dc.language.isoengen_US
dc.titleAnalysis of storm surge events along the Norwegian coasten_US
dc.title.alternativeAnalysis of storm surge events along the Norwegian coasten_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.volume11en_US
dc.source.journalFrontiers in Earth Scienceen_US
dc.identifier.doi10.3389/feart.2023.1037826
dc.identifier.cristin2129944
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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