Book 2.indb - US Climate Change Science Program

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Lynch-Stieglitz, and W.B. Curry, 2006: Gulf Streamdensity structure and transport during the past millennium. Nature,444, pp. 601–604.Lynch-Stieglitz, J., J.F. Adkins, W.B. Curry, T. Dokken, I.R. Hall,J.C. Herguera, J.J.-M. Hirschi, E.V. Ivanova, C. Kissel, O.Marchal, T.M. Marchitto, I.N. McCave, J.F. McManus, S. Mulitza,U. Ninnemann, F. Peeters, E.-F. Yu, and R. Zahn, 2007:Atlantic meridional overturning circulation during the LastGlacial Maximum. Science, 316(5821), pp. 66–69.Lynch-Stieglitz, J., W.B. Curry, D.W. Oppo, U.S. Ninneman,C.D. Charles, and J. Munson, 2006: Meridional overturningcirculation in the South Atlantic at the last glacial maximum.Geochemistry, Geophysics, Geosystems, 7, Q10N03,doi:10.1029/2005GC001226.Lynch-Stieglitz, J., W.B. Curry, and N. Slowey, 1999: WeakerGulf Stream in the Florida Straits during the Last Glacial Maximum.Nature, 402, pp. 644–648.Macrander, A., U. Send, H. Vadimarsson, S. Jónsson, andR.H. 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