{"refrec":{"BRefID":255271,"RR":"<b>Cimatoribus, A.; van Haren, H.</b> (2016). Estimates of the temperature flux-temperature gradient relation above a sea floor. <i>J. Fluid Mech. 793</i>: 504- 523. <a href=\"http://dx.doi.org/10.1017/jfm.2016.112\" target=\"_blank\">dx.doi.org/10.1017/jfm.2016.112</a>","BEntID":247274,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>J. Fluid Mech. 793</i>: 504- 523. <a href=\"https://dx.doi.org/10.1017/jfm.2016.112\" target=\"_blank\">https://dx.doi.org/10.1017/jfm.2016.112</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cimatoribus, A.; van Haren, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cimatoribus, A.; van Haren, H.","Englishabstract":"The relation between the ux of temperature (or buoyancy), the verti-cal temperature gradient and the height above the bottom, is investigatedin an oceanographic context, using high-resolution temperature measure-ments. The model for the evolution of a strati?ed layer by Balmforthet al. (1998) is reviewed and adapted to the case of a turbulent owabove a wall. Model predictions are compared to the average observa-tional estimates of the ux, exploiting a ux estimation method proposedby Winters & D'Asaro (1996). This estimation method enables the dis-entanglement of the dependence of the average ux on the height abovethe bottom and on the background temperature gradient. The classicalN-shaped ux-gradient relation is found in the observations. Model andobservations show similar qualitative behaviour, despite the strong sim-pli?cations used in the model. The results shed light on the modulationof the temperature ux by the presence of the boundary, and support theidea of a turbulent ux following a mixing-length argument in a strati?edow. Furthermore, the results support the use of Thorpe scales close to aboundary, if su?cient averaging is performed, suggesting that the Thorpescales are a?ected by the boundary in a similar way as the mixing length.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Estimates of the temperature flux-temperature gradient relation above a sea floor","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2016-04-26","DateCreate":"2016-04-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000372822600020","VABBcode":null,"OpenAcc":1,"DOI":"10.1017/jfm.2016.112"},"refs":null,"anarec":{"AnaID":255271,"PubliDate":2016,"Pagination":"504- 523","XtraPublOfAnaID":null,"ISBN":null,"Volume":"793","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43235,"SerRR":"Journal of Fluid Mechanics. 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