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dc.contributor.authorMalila, Mika Petteri
dc.contributor.authorBarbariol, Francesco
dc.contributor.authorBenetazzo, Alvise
dc.contributor.authorBreivik, Øyvind
dc.contributor.authorMagnusson, Anne Karin
dc.contributor.authorThomson, Jim
dc.contributor.authorWard, Brian
dc.date.accessioned2024-08-02T07:44:57Z
dc.date.available2024-08-02T07:44:57Z
dc.date.created2023-02-25T18:12:04Z
dc.date.issued2023
dc.identifier.issn0022-3670
dc.identifier.urihttps://hdl.handle.net/11250/3144178
dc.description.abstractWave crests of unexpected height and steepness pose a danger to activities at sea, and long-term field measurements provide important clues for understanding the environmental conditions that are conducive to their generation and behavior. We present a novel dataset of high-frequency laser altimeter measurements of the sea surface elevation gathered over a period of 18 years from 2003 to 2020 on an offshore platform in the central North Sea. Our analysis of crest height distributions in the dataset shows that mature, high sea states with high spectral steepness and narrow directional spreading exhibit crest height statistics that significantly deviate from standard second-order models. Conversely, crest heights in developing sea states with similarly high steepness but wide directional spread correspond well to second-order theory adjusted for broad frequency bandwidth. The long-term point time series measurements are complemented with space–time stereo video observations from the same location, collected during five separate storm events during the 2019/20 winter season. An examination of the crest dynamics of the space–time extreme wave crests in the stereo video dataset reveals that the crest speeds exhibit a slowdown localized around the moment of maximum crest elevation, in line with prevailing theory on nonlinear wave group dynamics. Extending on previously published observations focused on breaking crests, our results are consistent for both breaking and nonbreaking extreme crests. We show that wave crest steepness estimated from time series using the linear dispersion relation may overestimate the geometrically measured crest steepness by up to 25% if the crest speed slowdown is not taken into account.en_US
dc.language.isoengen_US
dc.publisherAMSen_US
dc.titleStatistical and Dynamical Characteristics of Extreme Wave Crests Assessed with Field Measurements from the North Seaen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2023 American Meteorological Societyen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1175/JPO-D-22-0125.1
dc.identifier.cristin2129253
dc.source.journalJournal of Physical Oceanographyen_US
dc.source.pagenumber509-531en_US
dc.relation.projectNorges forskningsråd: 300608en_US
dc.relation.projectNorges forskningsråd: 324227en_US
dc.relation.projectConoco Phillips: StereoWave projecten_US
dc.relation.projectEquinor: StereoWave projecten_US
dc.identifier.citationJournal of Physical Oceanography. 2023, 53 (2), 509-531.en_US
dc.source.volume53en_US
dc.source.issue2en_US


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