{"refrec":{"BRefID":135980,"RR":"<b>Ivins, E.R.</b> (2009). Ice sheet stability and sea level. <i>Science (Wash.) 324(5829)</i>: 888-889. <a href=\"https://dx.doi.org/10.1126/science.1173958\" target=\"_blank\">https://dx.doi.org/10.1126/science.1173958</a>","BEntID":129837,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 324(5829)</i>: 888-889. <a href=\"https://dx.doi.org/10.1126/science.1173958\" target=\"_blank\">https://dx.doi.org/10.1126/science.1173958</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ivins, E.R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ivins, E.R.","Englishabstract":"Volume changes in the Antarctic Ice Sheet are poorly understood, despite the importance of the ice sheet to sea-level and climate variability. Over both millennial and shorter time scales, net water influx to the ice sheet (mainly snow accumulation) nearly balances water loss through ice calving and basal ice shelf melting at the ice sheet margins (1). However, there may be times when parts of the West Antarctic Ice Sheet (WAIS) are lost to the oceans, thus raising sea levels. On page 901 of this issue, Bamber et al. 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