{"refrec":{"BRefID":30431,"RR":"<b>Loutre, M.F.; Berger, A.</b> (2000). No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO<sub>2</sub>. <i>Geophys. Res. Lett. 27(6)</i>: 783-786. <a href=\"https://dx.doi.org/10.1029/1999GL006081\" target=\"_blank\">https://dx.doi.org/10.1029/1999GL006081</a>","BEntID":30431,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 27(6)</i>: 783-786. <a href=\"https://dx.doi.org/10.1029/1999GL006081\" target=\"_blank\">https://dx.doi.org/10.1029/1999GL006081</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Loutre, M.F.; Berger, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Loutre, M.F.; Berger, A.","Englishabstract":"The relative impact of the CO<sub>2</sub> concentration on climate-over the last 200 kyr is investigated here using the Louvain-la-Neuve 2-dimension Northern Hemisphere (LLN 2-D NH) climate model forced by different constant insolations and the variable CO<sub>2</sub> concentration reconstructed from the Vostok ice-core record. Under such conditions the 100-kyr cycle in-the Northern Hemisphere ice volume cannot be reproduced. Either a warm orbit prevents the ice sheets from forming-or a present-day and colder orbits do not allow them tol:melt:after being formed. 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