共 8 条
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Synergistic feedbacks from ocean and vegetation on the African Monsoon response to Mid‐Holocene insolation[J] . P. Braconnot,S. Joussaume,O. Marti,N. de Noblet.Geophys. Res. Lett. . 1999 (16)
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East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea[J] . L Wang,M Sarnthein,H Erlenkeuser,J Grimalt,P Grootes,S Heilig,E Ivanova,M Kienast,C Pelejero,U Pflaumann.Marine Geology . 1999 (1)
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Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)[J] . S. Joussaume,K. E. Taylor,P. Braconnot,J. F. B. Mitchell,J. E. Kutzbach,S. P. Harrison,I. C. Prentice,A. J. Broccoli,A. Abe‐Ouchi,P. J. Bartlein,C. Bonfils,B. Dong,J. Guiot,K. Herterich,C. D. Hewitt,D. Jolly,J. W. Kim,A. Kislov,A. Kitoh,M. F. Loutre,V. Masson,B. McAvaney,N. McFarlane,N. de Noblet,W. R. Peltier,J. Y. Peterschmitt,D. Pollard,D. Rind,J. F. Royer,M. E. Sch
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The Greening of the Sahara during the Mid-Holocene: Results of an Interactive Atmosphere-Biome Model[J] . Global Ecology and Biogeography Letters . 1997 (5)
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Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene. JE Kutzbach,Z Liu. Science . 1997