{"refrec":{"BRefID":254724,"RR":"<b>Lear, C.H.; Lunt, D.J.</b> (2016). How Antarctica got its ice. <i>Science (Wash.) 352(6281)</i>: 34-35. <a href=\"http://dx.doi.org/10.1126/science.aad6284\" target=\"_blank\">http://dx.doi.org/10.1126/science.aad6284</a>","BEntID":246729,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 352(6281)</i>: 34-35. <a href=\"http://dx.doi.org/10.1126/science.aad6284\" target=\"_blank\">http://dx.doi.org/10.1126/science.aad6284</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lear, C.H.; Lunt, D.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lear, C.H.; Lunt, D.J.","Englishabstract":"Ice sheets such as those on Greenland and Antarctica today not only respond to changing climate but can also cause climate to change. Their sizes have fluctuated substantially in the past. 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