{"refrec":{"BRefID":362055,"RR":"<b>Docquier, D.; Vannitsem, S.; Ragone, F.; Wyser, K.; Liang, X.S.</b> (2022). Causal links between Arctic sea ice and its potential drivers based on the rate of information transfer. <i>Geophys. Res. Lett. 49(9)</i>: e2021GL095892. <a href=\"https://dx.doi.org/10.1029/2021GL095892\" target=\"_blank\">https://dx.doi.org/10.1029/2021GL095892</a>","BEntID":359771,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 49(9)</i>: e2021GL095892. <a href=\"https://dx.doi.org/10.1029/2021GL095892\" target=\"_blank\">https://dx.doi.org/10.1029/2021GL095892</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Docquier, D.; Vannitsem, S.; Ragone, F.; Wyser, K.; Liang, X.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Docquier, D. <i>et al.</i>","Englishabstract":"Arctic sea ice has substantially changed over the past four decades, with a large decrease in sea-ice area and volume. The exact causes of these changes are not entirely known. In our study, we make use of the Swedish Meteorological and Hydrological Institute Large Ensemble. This ensemble consists of 50 members realized with the EC-Earth3 global climate model and covers the period 1970-2100. We apply for the first time the Liang-Kleeman information flow method to analyze the cause-effect relationships between Arctic sea ice and its potential drivers. 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