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DOI	10.1126/science.253.5022.888
	Interpretation of snow-climate feedback as produced by 17 general circulation models
	Cess R.D.; Potter G.L.; Zhang M.-H.; Blanchet J.-P.; Chalita S.; Colman R.; Dazlich D.A.; Del Genio A.D.; Dymnikov V.; Galin V.; Jerrett D.; Keup E.; Lacis A.A.; Le Treut H.; Liang X.-Z.; Mahfouf J.-F.; McAvaney B.J.; Meleshko V.P.; Mitchell J.F.B.; Morcrette J.-J.; Norris P.M.; Randall D.A.; Rikus L.; Roeckner E.; Royer J.-F.; Schlese U.; Sheinin D.A.; Slingo J.M.; Sokolov A.P.; Taylor K.E.; Washington W.M.; Wetherald R.T.; Yagai I.
发表日期	1991
ISSN	0036-8075
起始页码	888
结束页码	892
卷号	253 期号:5022
英文摘要	Snow feedback is expected to amplify global warming caused by increasing concentrations of atmospheric greenhouse gases. The conventional explanation is that a warmer Earth will have less snow cover, resulting in a darker planet that absorbs more solar radiation. An intercomparison of 17 general circulation models, for which perturbations of sea surface temperature were used as a surrogate climate change, suggests that this explanation is overly simplistic. The results instead indicate that additional amplification or moderation may be caused both by cloud interactions and longwave radiation. One measure of this net effect of snow feedback was found to differ markedly among the 17 climate models, ranging from weak negative feedback in some models to strong positive feedback in others.
英文关键词	general circulation model; sea surface temperature; snow-climate feedback
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/243259
作者单位	Institute for Terrestrial and Planetary Atmospheres, State University of New York, Stony Brook, NY 11794, United States; Lawrence Livermore National Laboratory, Livermore, CA 94550, United States; Canadian Climate Centre, Downsview, Ont. M3H 574, Canada; Laboratoire de Météorologie Dynamique, 24 Rue Lhomond, 75231 Paris Cédex 05, France; Bureau of Meteorology Research Centre, GPO Box 1289K, Melbourne, Vic. 3001, Australia; Colorado State University, Fort Collins, CO 80523, United States; National Aeronautics and Space Administration (NASA), Goddard Institute for Space Studies, 2880 Broadway, New York, NY 10025, United States; Department of Numerical Mathematics, USSR Academy of Sciences, 29 Ryleeva Street, Moscow 119034, Russian Federation; Hadley Centre for Climate Prediction and Research, Meteorological Office, Bracknell, Berkshire RG12 2SZ, United Kingdom; Max Planck Institute for Meteorology, Bundestrasse 55, D2000, Hamburg 13, Germany; State University of New York, Albany, NY 12205, United States; Di...
推荐引用方式 GB/T 7714	Cess R.D.,Potter G.L.,Zhang M.-H.,et al. Interpretation of snow-climate feedback as produced by 17 general circulation models[J],1991,253(5022).
APA	Cess R.D..,Potter G.L..,Zhang M.-H..,Blanchet J.-P..,Chalita S..,...&Yagai I..(1991).Interpretation of snow-climate feedback as produced by 17 general circulation models.Science,253(5022).
MLA	Cess R.D.,et al."Interpretation of snow-climate feedback as produced by 17 general circulation models".Science 253.5022(1991).