{"refrec":{"BRefID":281763,"RR":"<b>Tynan, E.</b> (2016). Changing icescapes. <i>Nature Geoscience 9(12)</i>: 869-869. <a href=\"http://dx.doi.org/10.1038/ngeo2853\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2853</a>","BEntID":273778,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 9(12)</i>: 869-869. <a href=\"http://dx.doi.org/10.1038/ngeo2853\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2853</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Tynan, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Tynan, E.","Englishabstract":"The Antarctic land mass is surrounded by sea ice, which in winter can extend northwards for hundreds of kilometres. But the ice pack is not a continuous frozen icescape. 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