{"refrec":{"BRefID":114133,"RR":"<b>Meier, M.F.; Dyurgerov, M.B.; Rick, U.K.; O'Neel, S.; Pfeffer, W.T.; Anderson, R.S.; Anderson, S.P.; Glazovsky, A.F.</b> (2007). Glaciers dominate eustatic sea-level rise in the 21st century. <i>Science (Wash.) 317(5841)</i>: 1064-1067. <a href=\"https://dx.doi.org/10.1126/science.1143906\" target=\"_blank\">https://dx.doi.org/10.1126/science.1143906</a>","BEntID":106729,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 317(5841)</i>: 1064-1067. <a href=\"https://dx.doi.org/10.1126/science.1143906\" target=\"_blank\">https://dx.doi.org/10.1126/science.1143906</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Meier, M.F.; Dyurgerov, M.B.; Rick, U.K.; O'Neel, S.; Pfeffer, W.T.; Anderson, R.S.; Anderson, S.P.; Glazovsky, A.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Meier, M.F. <i>et al.</i>","Englishabstract":"Ice loss to the sea currently accounts for virtually all of sea-level rise not attributable to ocean warming; about 60% of the ice loss is from glaciers and ice caps rather than from the two ice sheets. The contribution of these smaller glaciers has accelerated over the last decade, in part due to dramatic thinning and retreat of marine-terminating glaciers associated with a dynamic instability generally not considered in mass balance/climate modeling. 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