{"refrec":{"BRefID":358978,"RR":"<b>Ruggiero, P.</b> (2004). Wave run-up on a high-energy dissipative beach. <i>J. Geophys. Res. 109(C6)</i>: C06025. <a href=\"https://dx.doi.org/10.1029/2003jc002160\" target=\"_blank\">https://dx.doi.org/10.1029/2003jc002160</a>","BEntID":356693,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 109(C6)</i>: C06025. <a href=\"https://dx.doi.org/10.1029/2003jc002160\" target=\"_blank\">https://dx.doi.org/10.1029/2003jc002160</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ruggiero, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ruggiero, P.","Englishabstract":"<span class=\"paraNumber\">[1] </span>Because of highly dissipative conditions and strong alongshore gradients in foreshore beach morphology, wave run-up data collected along the central Oregon coast during February 1996 stand in contrast to run-up data currently available in the literature. During a single data run lasting approximately 90 min, the significant vertical run-up elevation varied by a factor of 2 along the 1.6 km study site, ranging from 26 to 61% of the offshore significant wave height, and was found to be linearly dependent on the local foreshore beach slope that varied by a factor of 5. Run-up motions on this high-energy dissipative beach were dominated by infragravity (low frequency) energy with peak periods of approximately 230 s. Incident band energy levels were 2.5 to 3 orders of magnitude lower than the low-frequency spectral peaks and typically 96% of the run-up variance was in the infragravity band. A broad region of the run-up spectra exhibited an <i>f</i><sup>−4</sup> roll off, typical of saturation, extending to frequencies lower than observed in previous studies. The run-up spectra were dependent on beach slope with spectra for steeper foreshore slopes shifted toward higher frequencies than spectra for shallower foreshore slopes. At infragravity frequencies, run-up motions were coherent over alongshore length scales in excess of 1 km, significantly greater than decorrelation length scales on moderate to reflective beaches.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Wave run-up on a high-energy dissipative beach","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-13 01:31:57.216097","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2022-10-31","DateCreate":"2022-10-31","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000222777000001","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2003jc002160"},"refs":null,"anarec":{"AnaID":358978,"PubliDate":2004,"Pagination":"C06025","XtraPublOfAnaID":null,"ISBN":null,"Volume":"109","Issue":"C6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":90908,"SerRR":"Journal of Geophysical Research. 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