{"refrec":{"BRefID":344540,"RR":"<b>Bendtsen, J.; Rysgaard, S.; Carlson, D.F.; Meire, L.; Sejr, M.K.</b> (2021). Vertical mixing in stratified fjords near tidewater outlet glaciers along Northwest Greenland. <i>JGR: Oceans 126(8)</i>: e2020JC016898. <a href=\"https://dx.doi.org/10.1029/2020jc016898\" target=\"_blank\">https://dx.doi.org/10.1029/2020jc016898</a>","BEntID":341175,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>JGR: Oceans 126(8)</i>: e2020JC016898. <a href=\"https://dx.doi.org/10.1029/2020jc016898\" target=\"_blank\">https://dx.doi.org/10.1029/2020jc016898</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bendtsen, J.; Rysgaard, S.; Carlson, D.F.; Meire, L.; Sejr, M.K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bendtsen, J. <i>et al.</i>","Englishabstract":"<p>    Vertical mixing of upper water masses in Arctic fjords is important for    circulation and transport of nutrients and heat. However, the distribution    of turbulent mixing is poorly known. Here we present hydrographic and    microscale turbulence measurements from six fjords in Northwestern    (69°N–75°N) Greenland. Water mass distributions showed the presence of warm    bottom water of Atlantic origin in all fjord transects and a significant    modification of upper water masses in fjords with tidewater outlet    glaciers. Spatial and temporal distribution of turbulence in the fjordsshowed, in general, low rates of turbulent kinetic energy, ε (∼10    <sup>−9</sup> W kg<sup>−1</sup>), and strong stratification implies that    vertical exchange in the upper ∼200 m was relatively weak. However,    measurements within 2 km of the terminus of a tidewater outlet glaciershowed values of ε and inferred turbulent diffusion coefficients >10    <sup>−4</sup> m<sup>2</sup> s<sup>−1</sup> that were about two orders of    magnitude larger than elsewhere in the deep fjords. This elevated mixing    corresponded to comparatively large heat and salt fluxes. These    observations suggest that vertical mixing near tidewater outlet glaciers    results in localized mixing hot spots, likely due to subglacial discharge    and near-glacial current shear, that contribute significantly to vertical    exchange in the deep fjords.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Vertical mixing in stratified fjords near tidewater outlet glaciers along Northwest Greenland","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-06 01:34:35.866022","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2023-02-21","DateCreate":"2021-09-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000690758000014","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2020jc016898"},"refs":null,"anarec":{"AnaID":344540,"PubliDate":2021,"Pagination":"e2020JC016898","XtraPublOfAnaID":null,"ISBN":null,"Volume":"126","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":272092,"SerRR":"Journal of Geophysical Research-Oceans. 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