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  1. National Taiwan Ocean University Research Hub
  2. 海洋科學與資源學院
  3. 海洋環境資訊系
請用此 Handle URI 來引用此文件: http://scholars.ntou.edu.tw/handle/123456789/23894
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dc.contributor.authorYu-Chun Linen_US
dc.contributor.authorOey, Leoen_US
dc.date.accessioned2023-07-05T02:57:10Z-
dc.date.available2023-07-05T02:57:10Z-
dc.date.issued2020-02-
dc.identifier.issn0894-8755-
dc.identifier.issnWOS:000504734500001-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/23894-
dc.description.abstractAssessing trends of sea surface wave, wind, and coastal wave setup is of considerable scientific and practical importance in view of recent and projected long-term sea level rise due to global warming. Here we analyze global significant wave height (SWH) and wind data from 1993 to 2015 and a wave model to (i) calculate wave age and explain the causal, or the lack thereof, relationship between wave and wind trends; and (ii) estimate trends of coastal wave setup and its contributions to secular trends of relative sea level at coastal locations around the world. We show in-phase, increasing SWH and wind trends in regions dominated by younger waves, and decreasing SWH trends where older waves dominate and are unrelated to the local wind trends. In the central North Pacific where wave age is transitional, in-phase decreasing wave and wind trends are found over the west-northwestern region, but wave and wind trends are insignificantly correlated in the south-southeastern region; here, a reversed, upward momentum flux from wave to wind is postulated. We show that coastal wave setup depends primarily on open-ocean SWH but only weakly on wind, varying approximately like SWH/(wind speed)(1/5). The wave-setup trends are shown to be increasing along many coastlines where the local relative sea level trends are also increasing: the North and Irish Seas, Mediterranean Sea, East and South Asian seas, and eastern United States, exacerbating the potential for increased floods along these populated coastlines.en_US
dc.language.isoen_USen_US
dc.publisherAMER METEOROLOGICALen_US
dc.relation.ispartofJournal of Climateen_US
dc.subjectWind wavesen_US
dc.subjectSea stateen_US
dc.subjectSea levelen_US
dc.subjectMultidecadal variabilityen_US
dc.subjectTrendsen_US
dc.subjectWind effectsen_US
dc.subjectGLACIAL ISOSTATIC-ADJUSTMENTen_US
dc.subjectSOUTHERN ANNULAR MODEen_US
dc.subjectPOSTGLACIAL UPLIFTen_US
dc.subjectSUMMER MONSOONen_US
dc.subjectWINTER MONSOONen_US
dc.subjectNORTH-ATLANTICen_US
dc.subjectPACIFIC COASTen_US
dc.subjectLEVEL RISEen_US
dc.subjectVARIABILITYen_US
dc.subjectTIDEen_US
dc.titleGlobal Trends of Sea Surface Gravity Wave, Wind, and Coastal Wave Setupen_US
dc.typejournal articleen_US
dc.identifier.doi10.1175/JCLI-D-19-0347.1-
dc.relation.journalvolume33en_US
dc.relation.journalissue3en_US
dc.relation.pages769-785en_US
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.cerifentitytypePublications-
item.languageiso639-1en_US-
item.fulltextno fulltext-
item.grantfulltextnone-
item.openairetypejournal article-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptDepartment of Marine Environmental Informatics-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
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