{"refrec":{"BRefID":333320,"RR":"<b>Charette, M.A.; Kipp, L.E.; Jensen, L.T.; Dabrowski, J.S.; Whitmore, L.M.; Fitzsimmons, J.N.; Williford, T.; Ulfsbo, A.; Jones, E.; Bundy, R.M.; Vivancos, S.M.; Pahnke, K.; John, S.G.; Xiang, Y.; Hatta, M.; Petrova, M.V.; Heimbürger‐Boavida, L.‐E.; Bauch, D.; Newton, R.; Pasqualini, A.; Agather, A.M.; Amon, R.M.W.; Anderson, R.F.; Andersson, P.S.; Benner, R.; Bowman, K.L.; Edwards, R.L.; Gdaniec, S.; Gerringa, L.J.A.; González, A.G.; Granskog, M.; Haley, B.; Hammerschmidt, C.R.; Hansell, D.A.; Henderson, P.B.; Kadko, D.C.; Kaiser, K.; Laan, P.; Lam, P.J.; Lamborg, C.H.; Levier, M.; Li, X.; Margolin, A.R.; Measures, C.; Middag, R.; Millero, F.J.; Moore, W.S.; Paffrath, R.; Planquette, H.; Rabe, B.; Reader, H.; Rember, R.; Rijkenberg, M.J.A.; Roy‐Barman, M.; Rutgers van der Loeff, M.; Saito, M.; Schauer, U.; Schlosser, P.; Sherrell, R.M.; Shiller, A.M.; Slagter, H.; Sonke, J.E.; Stedmon, C.; Woosley, R.J.; Valk, O.; Ooijen, J.; Zhang, R.</b> (2020). The Transpolar Drift as a source of riverine and shelf‐derived trace elements to the central Arctic Ocean. <i>JGR: Oceans 125(5)</i>: e2019JC015920. <a href=\"https://doi.org/10.1029/2019jc015920\" target=\"_blank\">https://doi.org/10.1029/2019jc015920</a>","BEntID":326932,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>JGR: Oceans 125(5)</i>: e2019JC015920. <a href=\"https://doi.org/10.1029/2019jc015920\" target=\"_blank\">https://doi.org/10.1029/2019jc015920</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Charette, M.A.; Kipp, L.E.; Jensen, L.T.; Dabrowski, J.S.; Whitmore, L.M.; Fitzsimmons, J.N.; Williford, T.; Ulfsbo, A.; Jones, E.; Bundy, R.M.; Vivancos, S.M.; Pahnke, K.; John, S.G.; Xiang, Y.; Hatta, M.; Petrova, M.V.; Heimbürger‐Boavida, L.‐E.; Bauch, D.; Newton, R.; Pasqualini, A.; Agather, A.M.; Amon, R.M.W.; Anderson, R.F.; Andersson, P.S.; Benner, R.; Bowman, K.L.; Edwards, R.L.; Gdaniec, S.; Gerringa, L.J.A.; González, A.G.; Granskog, M.; Haley, B.; Hammerschmidt, C.R.; Hansell, D.A.; Henderson, P.B.; Kadko, D.C.; Kaiser, K.; Laan, P.; Lam, P.J.; Lamborg, C.H.; Levier, M.; Li, X.; Margolin, A.R.; Measures, C.; Middag, R.; Millero, F.J.; Moore, W.S.; Paffrath, R.; Planquette, H.; Rabe, B.; Reader, H.; Rember, R.; Rijkenberg, M.J.A.; Roy‐Barman, M.; Rutgers van der Loeff, M.; Saito, M.; Schauer, U.; Schlosser, P.; Sherrell, R.M.; Shiller, A.M.; Slagter, H.; Sonke, J.E.; Stedmon, C.; Woosley, R.J.; Valk, O.; Ooijen, J.; Zhang, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Charette, M.A. <i>et al.</i>","Englishabstract":"A major surface circulation feature of the Arctic Ocean is the Transpolar    Drift (TPD), a current that transports river‐influenced shelf water from    the Laptev and East Siberian Seas toward the center of the basin and Fram    Strait. In 2015, the international GEOTRACES program included a    high‐resolution pan‐Arctic survey of carbon, nutrients, and a suite of    trace elements and isotopes (TEIs). The cruises bisected the TPD at two    locations in the central basin, which were defined by maxima in meteoric    water and dissolved organic carbon concentrations that spanned 600 km    horizontally and ~25–50 m vertically. Dissolved TEIs such as Fe, Co, Ni,    Cu, Hg, Nd, and Th, which are generally particle‐reactive but can be    complexed by organic matter, were observed at concentrations much higher    than expected for the open ocean setting. Other trace element    concentrations such as Al, V, Ga, and Pb were lower than expected due to    scavenging over the productive East Siberian and Laptev shelf seas. Using a    combination of radionuclide tracers and ice drift modeling, the transport    rate for the core of the TPD was estimated at 0.9 ± 0.4 Sv (10<sup>6</sup>    m<sup>3</sup> s<sup>−1</sup>). This rate was used to derive the mass flux    for TEIs that were enriched in the TPD, revealing the importance of lateral    transport in supplying materials beneath the ice to the central Arctic    Ocean and potentially to the North Atlantic Ocean via Fram Strait.    Continued intensification of the Arctic hydrologic cycle and permafrost    degradation will likely lead to an increase in the flux of TEIs into the    Arctic Ocean.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The Transpolar Drift as a source of riverine and shelf‐derived trace elements to the central Arctic Ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:32:33.884703","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Arctic Ocean; Transpolar Drift; trace elements; carbon; nutrients; GEOTRACES]","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2021-02-03","DateCreate":"2021-02-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000548601000017","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2019jc015920"},"refs":null,"anarec":{"AnaID":333320,"PubliDate":2020,"Pagination":"e2019JC015920","XtraPublOfAnaID":null,"ISBN":null,"Volume":"125","Issue":"5","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":272092,"SerRR":"Journal of Geophysical Research-Oceans. 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