On the origin of the ice ages

Part of book or chapter of book English OPEN
Oerlemans, J.;
(1984)
  • Subject:
    arxiv: Physics::Geophysics | Physics::Atmospheric and Oceanic Physics | Astrophysics::Earth and Planetary Astrophysics

Ice sheet dynamics provide a possible explanation for the 100 kyr power in climatic records. Some numerical experiments presented here show that even the transition from an essentially ice-free earth to a glacial can be produced by a northern hemisphere ice-sheet model,... View more
  • References (7)

    1. Berger, A. : 1981, Climatic Variations and Variability : Facts and Theories, 795pp., Reidel Publ. Company, Holland.

    2. Oerlemans, J. : 1980, Nature 287, pp. 430-432.

    3. Birchfield, G.E., Weertman, J., and Lunde, A.T. : 1981, Quaternary Research 15, pp. 126-142.

    4. Pollard, D. : 1982, Nature 292, pp. 233-235.

    5. Oerlemans, J. : 1982, Climatic Change 4, pp. 353-374.

    6. Shackleton, N.J., and Opdyke, N.D. : 1976, Geol. Soc. Am. Mem. 145, pp. 449-464.

    7. Hooghiemstra, H. : 1984, in : "Milankovitch and Climate", A. Berger, J. Imbrie, J. Hays, G. Kukla, B. Saltzman (Eds), Reidel Publ. Company, Holland. This volume, p. 371.

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