{"refrec":{"BRefID":284788,"RR":"<b>van Haren, H.</b> (2017). Exploring the vertical extent of breaking internal wave turbulence above deep-sea topography. <i>Dyn. Atmos. Oceans 77</i>: 89–99. <a href=\"https://dx.doi.org/10.1016/j.dynatmoce.2017.01.002\" target=\"_blank\">https://dx.doi.org/10.1016/j.dynatmoce.2017.01.002</a>","BEntID":276812,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Dyn. Atmos. Oceans 77</i>: 89–99. <a href=\"https://dx.doi.org/10.1016/j.dynatmoce.2017.01.002\" target=\"_blank\">https://dx.doi.org/10.1016/j.dynatmoce.2017.01.002</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Haren, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van Haren, H.","Englishabstract":"A mooring equipped with 200 high-resolution temperature sensors between 6 and 404 m above the bottom was moored in 1890 m water depth above a steep, about 10° slope of Mount Josephine, NE-Atlantic. The sensors have a precision of less than 0.5 mK. They are synchronized via induction every 4 h so that the 400 m range is measured to within 0.02 s, every 1 s. Thin cables and elliptical buoyancy assured vertical mooring motions to be smaller than 0.1 m under maximum 0.2 m s−1 current speeds. The local bottom slope is supercritical for semidiurnal internal tides by a factor of two. Exploring a one-month record in detail, the observations show: 1/semidiurnal tidal dominance in variations of dissipation rate ε, eddy diffusivity Kz and temperature, but no significant correlation between the records of ε and total kinetic energy, 2/a variation with time over four orders of magnitude of 100-m vertically averaged ε, 3/a local minimum in density stratification between 50 and 100 m above the bottom, 4/a gradual decrease in daily or longer averaged ε and Kz by one order of magnitude over a vertical distance of 250 m, upwards from 150 m above the bottom, 5/monthly mean values of <[ε]> = 2 ± 0.5 × 10−7 m2 s−3, <[Kz]> = 8 ± 3 × 10−3 m2 s−1 averaged over the lower 150 m above the bottom.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Exploring the vertical extent of breaking internal wave turbulence above deep-sea topography","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":"Internal wave turbulence; Sloping ocean topography; Wave breaking; 400 m high mooring line; High-resolution temperature sensors ","OtherDescriptors":null,"Notes":null,"AnaPub":2017,"MonPub":null,"DateUpdate":"2017-12-21","DateCreate":"2017-05-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000398874400008","VABBcode":null,"OpenAcc":1,"DOI":"10.1016/j.dynatmoce.2017.01.002"},"refs":null,"anarec":{"AnaID":284788,"PubliDate":2017,"Pagination":"89–99","XtraPublOfAnaID":null,"ISBN":null,"Volume":"77","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42803,"SerRR":"Dynamics of Atmospheres and Oceans. 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