{"refrec":{"BRefID":367027,"RR":"<b>Van Achter, G.; Fichefet, T.; Goosse, H.; Pelletier, C.; Haubner, K.; Pattyn, F.</b> (2023). Ocean–ice sheet coupling in the Totten Glacier Area, East Antarctica: analysis of the feedbacks and their response to a sudden ocean warming. <i>Geosciences 13(4)</i>: 106. <a href=\"https://dx.doi.org/10.3390/geosciences13040106\" target=\"_blank\">https://dx.doi.org/10.3390/geosciences13040106</a>","BEntID":364751,"PublicFlag":1,"CheckedFlag":1,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Geosciences 13(4)</i>: 106. <a href=\"https://dx.doi.org/10.3390/geosciences13040106\" target=\"_blank\">https://dx.doi.org/10.3390/geosciences13040106</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Achter, G.; Fichefet, T.; Goosse, H.; Pelletier, C.; Haubner, K.; Pattyn, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Achter, G. <i>et al.</i>","Englishabstract":"We coupled together high-resolution versions of the ocean-sea ice model NEMO and the ice sheet model BISICLES configured to the Totten Glacier area and ran a series of simulations over the recent past (1995-2014) and under warming conditions (2081-2100; SSP4-4.5) with NEMO in stand-alone mode and with the coupled model to assess the effects of the coupling. During the recent past, the ocean-ice sheet coupling has increased the time-averaged value of the basal melt rate in both the Totten and Moscow University ice shelf cavities by 6.7% and 14.2%, respectively. The relationship between the changes in ice shelf thickness and ice shelf basal melt rate suggests that the effect of the coupling is not a linear response to the melt rate but rather a more complex response, driven partly by the dynamical component of the ice sheet model. The response of the ice sheet-ocean coupling due to the ocean warming is a 10% and 3% basal melt rate decrease in the Totten and Moscow University ice shelf cavities, respectively. This indicates that the ocean-ice sheet coupling under climate warming conditions dampens the basal melt rates. Our study highlights the importance of incorporating ocean-ice sheet coupling in climate simulations, even over short time periods.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Ocean–ice sheet coupling in the Totten Glacier Area, East Antarctica: analysis of the feedbacks and their response to a sudden ocean warming","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-09-25 01:36:50.712317","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"NEMO–BISICLES coupling; basal melt rates; ocean–ice shelf interactions","OtherDescriptors":null,"Notes":null,"AnaPub":2023,"MonPub":null,"DateUpdate":"2025-09-18","DateCreate":"2023-09-18","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000981020700001","VABBcode":null,"OpenAcc":1,"DOI":"10.3390/geosciences13040106"},"refs":null,"anarec":{"AnaID":367027,"PubliDate":2023,"Pagination":"106","XtraPublOfAnaID":null,"ISBN":null,"Volume":"13","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":305019,"SerRR":"Geosciences. 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