{"refrec":{"BRefID":257854,"RR":"<b>Goosse, H.; Arzel, O.; Bitz, C.; de Montety, A.; Vancoppenolle, M.</b> (2009). Increased variability of the Arctic summer ice extent in a warmer climate. <i>Geophys. Res. Lett. 36(23)</i>. <a href=\"http://dx.doi.org/10.1029/2009GL040546\" target=\"_blank\">dx.doi.org/10.1029/2009GL040546</a>","BEntID":249864,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 36(23)</i>. <a href=\"https://dx.doi.org/10.1029/2009GL040546\" target=\"_blank\">https://dx.doi.org/10.1029/2009GL040546</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Goosse, H.; Arzel, O.; Bitz, C.; de Montety, A.; Vancoppenolle, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Goosse, H. <i>et al.</i>","Englishabstract":"Simulations performed with general circulation models and a model of intermediate complexity show that the variability of the September sea ice extent in the Arctic of the 21st century increases first when the mean extent decreases from present-day values. A maximum of the variance is found when the mean September ice extent is around 3 million km<sup>2</sup>. For lower extents, the variance declines with the mean extent. The behavior is clearly different in Antarctica where the variance always decreases as the mean ice extent decreases, following roughly a square-root law compatible with very simple geometric arguments. Several mechanisms are responsible for the non-linear behavior of the Arctic. 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