{"refrec":{"BRefID":340199,"RR":"<b>Minowa, M.; Sugiyama, S.; Ito, M.; Yamane, S.; Aoki, S.</b> (2021). Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica. <i>Nature Comm. 12(1)</i>: 4209. <a href=\"https://dx.doi.org/10.1038/s41467-021-23534-w\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-021-23534-w</a>","BEntID":336834,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 12(1)</i>: 4209. <a href=\"https://dx.doi.org/10.1038/s41467-021-23534-w\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-021-23534-w</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Minowa, M.; Sugiyama, S.; Ito, M.; Yamane, S.; Aoki, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Minowa, M. <i>et al.</i>","Englishabstract":"Basal melting of ice shelves is considered to be the principal driver of recent ice mass loss in Antarctica. Nevertheless, in-situ oceanic data covering the extensive areas of a subshelf cavity are sparse. Here we show comprehensive structures of temperature, salinity and current measured in January 2018 through four boreholes drilled at a ~3-km-long ice shelf of Langhovde Glacier in East Antarctica. The measurements were performed in 302–12 m-thick ocean cavity beneath 234–412 m-thick ice shelf. The data indicate that Modified Warm Deep Water is transported into the grounding zone beneath a stratified buoyant plume. Water at the ice-ocean interface was warmer than the in-situ freezing point by 0.65–0.95°C, leading to a mean basal melt rate estimate of 1.42 m a<sup>−1</sup>. Our measurements indicate the existence of a density-driven water circulation in the cavity beneath the ice shelf of Langhovde Glacier, similar to that proposed for warm-ocean cavities of larger Antarctic ice shelves.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-16 01:33:26.751094","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-07-22","DateCreate":"2021-07-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000674487100008","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41467-021-23534-w"},"refs":null,"anarec":{"AnaID":340199,"PubliDate":2021,"Pagination":"4209","XtraPublOfAnaID":null,"ISBN":null,"Volume":"12","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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