{"refrec":{"BRefID":350712,"RR":"<b>Patterson, M.O.; Levy, R.H.; Kulhanek, D.K.; van de Flierdt, T.; Horgan, H.; Dunbar, G.B.; Naish, T.R.; Ash, J.; Pyne, A.; Mandeno, D.; Winberry, P.; Harwood, D.M.; Florindo, F.; Jimenez-Espejo, F.J.; Läufer, A.; Yoo, K.-C.; Seki, O.; Stocchi, P.; Klages, J.P.; Lee, J.I.; Colleoni, F.; Suganuma, Y.; Gasson, E.; Ohneiser, C.; Flores, J.-A.; Try, D.; Kirkman, R.; Koch, D.; the SWAIS 2C Science Team</b> (2022). Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C). <i>Sci. Drill. 30</i>: 101-112. <a href=\"https://dx.doi.org/10.5194/sd-30-101-2022\" target=\"_blank\">https://dx.doi.org/10.5194/sd-30-101-2022</a>","BEntID":348408,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Sci. Drill. 30</i>: 101-112. <a href=\"https://dx.doi.org/10.5194/sd-30-101-2022\" target=\"_blank\">https://dx.doi.org/10.5194/sd-30-101-2022</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Patterson, M.O.; Levy, R.H.; Kulhanek, D.K.; van de Flierdt, T.; Horgan, H.; Dunbar, G.B.; Naish, T.R.; Ash, J.; Pyne, A.; Mandeno, D.; Winberry, P.; Harwood, D.M.; Florindo, F.; Jimenez-Espejo, F.J.; Läufer, A.; Yoo, K.-C.; Seki, O.; Stocchi, P.; Klages, J.P.; Lee, J.I.; Colleoni, F.; Suganuma, Y.; Gasson, E.; Ohneiser, C.; Flores, J.-A.; Try, D.; Kirkman, R.; Koch, D.; the SWAIS 2C Science Team","OrigTitleTranslFlag":0,"Authorstringtrunc":"Patterson, M.O. <i>et al.</i>","Englishabstract":"<p>    The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise    global sea level by 4.3 m if completely melted. The unknown response of the    WAIS to future warming remains a significant challenge for numerical models    in quantifying predictions of future sea level rise. Sea level rise is one    of the clearest planet-wide signals of human-induced climate change. The    Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 <sup>∘</sup>C    (SWAIS 2C) Project aims to understand past and current drivers and    thresholds of WAIS dynamics to improve projections of the rate and size of    ice sheet changes under a range of elevated greenhouse gas levels in the    atmosphere as well as the associated average global temperature scenarios    to and beyond the +2 <sup>∘</sup>C target of the Paris Climate Agreement.</p><p>    Despite efforts through previous land and ship-based drilling on and along    the Antarctic margin, unequivocal evidence of major WAIS retreat or    collapse and its causes has remained elusive. To evaluate and plan for the    interdisciplinary scientific opportunities and engineering challenges that    an International Continental Drilling Program (ICDP) project along the    Siple coast near the grounding zone of the WAIS could offer (Fig. 1),    researchers, engineers, and logistics providers representing 10 countries    held a virtual workshop in October 2020. This international partnership    comprised of geologists, glaciologists, oceanographers, geophysicists,    microbiologists, climate and ice sheet modelers, and engineers outlined    specific research objectives and logistical challenges associated with the    recovery of Neogene and Quaternary geological records from the West    Antarctic interior adjacent to the Kamb Ice Stream and at Crary Ice Rise.    New geophysical surveys at these locations have identified drilling targets    in which new drilling technologies will allow for the recovery of up to    200 m of sediments beneath the ice sheet. Sub-ice-shelf records have so far    proven difficult to obtain but are critical to better constrain marine ice    sheet sensitivity to past and future increases in global mean surface    temperature up to 2 <sup>∘</sup>C above pre-industrial levels. Thus, the    scientific and technological advances developed through this program will    enable us to test whether WAIS collapsed during past intervals of warmth    and determine its sensitivity to a +2 <sup>∘</sup>C global warming    threshold (UNFCCC, 2015).</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-09 01:32:20.942535","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-03-31","DateCreate":"2022-03-31","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000763332900001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/sd-30-101-2022"},"refs":null,"anarec":{"AnaID":350712,"PubliDate":2022,"Pagination":"101-112","XtraPublOfAnaID":null,"ISBN":null,"Volume":"30","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":199101,"SerRR":"Scientific Drilling. 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