{"refrec":{"BRefID":334342,"RR":"<b>van Haren, H.; Brussaard, C.P.D.; Gerringa, L.J.A.; van Manen, M.H.; Middag, R.; Groenewegen, R.</b> (2021). Diapycnal mixing across the photic zone of the NE Atlantic. <i>Ocean Sci. 17</i>: 301-318. <a href=\"https://doi.org/10.5194/os-17-301-2021\" target=\"_blank\">https://doi.org/10.5194/os-17-301-2021</a>","BEntID":330898,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Ocean Sci. 17</i>: 301-318. <a href=\"https://doi.org/10.5194/os-17-301-2021\" target=\"_blank\">https://doi.org/10.5194/os-17-301-2021</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Haren, H.; Brussaard, C.P.D.; Gerringa, L.J.A.; van Manen, M.H.; Middag, R.; Groenewegen, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van Haren, H. <i>et al.</i>","Englishabstract":"<p>    Variable physical conditions such as vertical turbulent exchange, internal    wave, and mesoscale eddy action affect the availability of light and    nutrients for phytoplankton (unicellular algae) growth. It is hypothesized    that changes in ocean temperature may affect ocean vertical density    stratification, which may hamper vertical exchange. In order to quantify    variations in physical conditions in the northeast Atlantic Ocean, wesampled a latitudinal transect along 17 ± 5<sup>∘</sup> W between 30 and 63    <sup>∘</sup> N in summer. A shipborne conductivity–temperature–depth (CTD)    instrumented package was used with a custom-made modification of the pump    inlet to minimize detrimental effects of ship motions on its data.    Thorpe-scale analysis was used to establish turbulence values for the upper    500 m from three to six profiles obtained in a short CTD yo-yo, 3 to 5 h    after local sunrise. From south to north, average temperature decreased    together with stratification while turbulence values weakly increased or    remained constant. Vertical turbulent nutrient fluxes did not vary    significantly with stratification and latitude. This apparent lack of    correspondence between turbulent mixing and temperature is likely due to    internal waves breaking (increased stratification can support more internal    waves), acting as a potential feedback mechanism. As this feedback    mechanism mediates potential physical environment changes in temperature,    global surface ocean warming may not affect the vertical nutrient fluxes to    a large degree. We urge modellers to test this deduction as it could imply    that the future summer phytoplankton productivity in stratified    oligotrophic waters would experience little alterations in nutrient input    from deeper waters.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Diapycnal mixing across the photic zone of the NE Atlantic","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:32:34.150350","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-03-09","DateCreate":"2021-03-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000620895200001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/os-17-301-2021"},"refs":null,"anarec":{"AnaID":334342,"PubliDate":2021,"Pagination":"301-318","XtraPublOfAnaID":null,"ISBN":null,"Volume":"17","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":105415,"SerRR":"Ocean Science. 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ISSN 1812-0784; e-ISSN 1812-0792","StandardTitleSer":"Ocean Science","ISSN":"1812-0784","AbbrevSer":"Ocean Sci.","StandardTitleMon":null,"StartPage":301,"Pages":18,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"van Haren","Firstname":"Hans","Initials":"H.","Affiliation":"OCS","Discriminator":null,"CorporateFlag":0,"BEntID":330898,"AutID":211311,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"OCS","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; Ocean Sciences","ORCID":"0000-0001-8041-8121","PersID":29754,"InsID":13654},{"AutName":"Brussaard","Firstname":"Corina","Initials":"C.P.D.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":330898,"AutID":207976,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"MMB","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; 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