{"refrec":{"BRefID":291313,"RR":"<b>Langlais, C.E.; Lenton, A.; Matear, R.; Monselesan, D.; Legresy, B.; Cougnon, E.; Rintoul, S.</b> (2017). Stationary Rossby waves dominate subduction of anthropogenic carbon in the Southern Ocean. <i>NPG Scientific Reports 7(1)</i>: 10 pp. <a href=\"https://dx.doi.org/10.1038/s41598-017-17292-3\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-017-17292-3</a>","BEntID":283356,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>NPG Scientific Reports 7(1)</i>: 10 pp. <a href=\"https://dx.doi.org/10.1038/s41598-017-17292-3\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-017-17292-3</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Langlais, C.E.; Lenton, A.; Matear, R.; Monselesan, D.; Legresy, B.; Cougnon, E.; Rintoul, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Langlais, C.E. <i>et al.</i>","Englishabstract":"The Southern Ocean has taken up more than 40% of the total anthropogenic carbon (C-ant) stored in the oceans since the preindustrial era, mainly in subantarctic mode and intermediate waters (SAMW-AAIW). However, the physical mechanisms responsible for the transfer of C-ant into the ocean interior remain poorly understood. Here, we use high resolution (1/10 degrees) ocean simulations to investigate these mechanisms at the SAMW-AAIW subduction hotspots. Mesoscale Stationary Rossby Waves (SRWs), generated where the Antarctic Circumpolar Current interacts with topography, make the dominant contribution to the C-ant transfer in SAMW-AAIW in the Indian and Pacific sectors (66% and 95% respectively). Eddy-resolving simulations reproduce the observed C-ant sequestration in these layers, while lower spatial resolution models, that do not reproduce SRWs, underestimate the inventory of C-ant in these layers by 40% and overestimate the storage in denser layers. A key implication is that climate model simulations, that lack sufficient resolution to represent sequestration by SRWs, are therefore likely to overestimate the residence time of C-ant in the ocean, with implications for simulated rates of climate change.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Stationary Rossby waves dominate subduction of anthropogenic carbon in the Southern Ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-13 01:31:34.198556","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2017,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2017-12-08","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000417135800015","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41598-017-17292-3"},"refs":null,"anarec":{"AnaID":291313,"PubliDate":2017,"Pagination":"10 pp","XtraPublOfAnaID":null,"ISBN":null,"Volume":"7","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":208093,"SerRR":"Scientific Reports (Nature Publishing Group). Nature Publishing Group: London.  ISSN 2045-2322; e-ISSN 2045-2322","StandardTitleSer":"Scientific Reports (Nature Publishing Group)","ISSN":"2045-2322","AbbrevSer":"NPG Scientific Reports","StandardTitleMon":null,"StartPage":null,"Pages":null,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Langlais","Firstname":null,"Initials":"C.E.","Affiliation":"CSIRO Oceans & Atmosphere, Hobart, Tas 7000, Australia.","Discriminator":null,"CorporateFlag":0,"BEntID":283356,"AutID":300464,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Lenton","Firstname":null,"Initials":"A.","Affiliation":"CSIRO Oceans & Atmosphere, Hobart, Tas 7000, 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