{"refrec":{"BRefID":312024,"RR":"<b>Larour, E.; Seroussi, H.; Adhikari, S.; Ivins, E.R.; Caron, L.; Morlighem, M.; Schlegel, N.</b> (2019). Slowdown in Antarctic mass loss from solid Earth and sea-level feedbacks. <i>Science (Wash.) 364(6444)</i>: eaav7908. <a href=\"https://dx.doi.org/10.1126/science.aav7908\" target=\"_blank\">https://dx.doi.org/10.1126/science.aav7908</a>","BEntID":304388,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 364(6444)</i>: eaav7908. <a href=\"https://dx.doi.org/10.1126/science.aav7908\" target=\"_blank\">https://dx.doi.org/10.1126/science.aav7908</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Larour, E.; Seroussi, H.; Adhikari, S.; Ivins, E.R.; Caron, L.; Morlighem, M.; Schlegel, N.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Larour, E. <i>et al.</i>","Englishabstract":"The rise in sea level that is occurring from the melting of Antarctica is only going to accelerate as climate warms. However, Larour et al. report that crustal uplift in the Amundsen Sea sector is helping to reduce grounding line retreat, thereby stabilizing the ice sheet and slowing its rate of mass loss (see the Perspective by Steig). 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