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Joussaume, S.; Taylor, K. E.; Braconnot, P.; Mitchell, J. F. B.; Kutzbach, J. E.; Harrison, S. P.; Prentice, I. C.; Broccoli, A. J.; Abe-Ouchi, A.; Bartlein, P. J.; Bonfils, C.; Dong, B.; Guiot, J.; Herterich, K.; Hewitt, C. D.; Jolly, D.; Kim, J. W.; Kislov, A.; Kitoh, A.; Loutre, M. F.; Masson, V.; McAvaney, B.; McFarlane, N.; de Noblet, N.; Peltier, W. R.; Peterschmitt, J. Y.; Pollard, D.; Rind, D.; Royer, J. F.; Schlesinger, M. E.; Syktus, J.; Thompson, S.; Valdes, P.; Vettoretti, G.; Webb, R. S.; Wyputta, U.
Geophysical research letters, 1 April 1999, Letnik: 26, Številka: 7Journal Article
Amplification of the northern hemisphere seasonal cycle of insolation during the mid‐Holocene causes a northward shift of the main regions of monsoon precipitation over Africa and India in all 18 simulations conducted for the Paleoclimate Modeling Intercomparison Project (PMIP). Differences among simulations are related to differences in model formulation. Despite qualitative agreement with paleoecological estimates of biome shifts, the magnitude of the monsoon increases over northern Africa are underestimated by all the models.
