References

Berger, A. (1978). Long-term variations of daily insolation and Quaternary climatic change. Jour, of Aim Sei., 35, 2362-2367.

Fiercer, A,, Fichefet, Th., Gallce, H., Tricot, Ch., and van Ypersele, J, P. (l^Z). Entering the glaciation with a 2-L) coupled climate model, Quat Sei. Rev., 11, 4KI 493.

Berger. V. (1998). Milankovitch theory and climate. Rev. Geophys,, 26, 624 057.

Berger, A., Loutre, M F., and Gal lee, H, (1998). Sensitivity of the LLN climate model to the astronomical and CO2 forcings over the last 200 ky. Climate Dynamics, 14, 615-629.

MaTepwa/i, 3aL4WLneHHbifr aBTopcKMM npaBOM

Milankovitch, M. (1920). Théorie mathématique Jes phenomena therm tques pwJuits parla radiation solarte. üauihier-Villars, Paris, 338 pp,

Mitchell, J. F. 1 i. (1977). Met 0 21) Tech. Note 11/100 Meteorological Office, Bracknell,

Mitchell, J. F. B., Grahame, N, S,, and Necdham, K. 1 E (1988), Climate simulations for 9000 years before present: seasonal variations and the effect of the Laurentide Ice Sheet. Jour, of Geophys. Res., 93t 8283-8303.

Modey,J. J., and Dworetzky, B. A, (1993). Holoterve temperature patterns in the South Atlantic In Global Climates since the Last GlacialMaximum, eds, H. E. Wright Jr, J. E. Kutzbach, T. Webb, 1 IK W, E Ruddiman, F. A. Street-Perrott, and P J, Bart km (Minneapolis, MM: University of Minnesota Press), 125-135,

Otto-Bliesrter, B. I(1999). El NííWEa Niña and Sahel precipitation during the middle I loloccnc. Gcophys, Res, Eett,, 26, 87-90,

Phillips, P. J,, and Held, I, M (1994). The response of orbital perturbations in an atmospheric model coupled to a slab ocean. Jour of Clim. 7,767-782.

Pollard, l>, Bcrgengrtn, J. C, Still well-Sol let, E, M., Fclzer, B., and Thompson, S. L. (1998), Climate simulations for 10000 and 6000 years BP using the GENESIS global climate model, Paleoclimatcs, 2, 183-218.

Prell, W. E. (1984a). Variation of monsoonal upwelling; a response to changing solar radiation. Climate Processes and Climate Sensitivity, Gcophys. Monogr, Ser., vol 29, AGU, Washington, DC

PreN, W. E. (1984b). Monsoonal climate of the Arabian sea during the late Quaternary; a response to solar radiation. In Milankovitch and Climate t cds. A. Berger, J. Imbrie, J. Hays, G. K.ukla, and II. Salt/man (D. Reidel, Htngman, MA), 349-366,

Raynaud, D., Jouzel, J„ Barnola, J. M,, Chappelaz, J., Delmas, R-, and Lorius, C. (1993). The ice record of greenhouse gases. Science, 259,926-934.

Ritchie, J. C, Cwynar, L, C., and Spear, R. W. (1983). Evidence from north-west Canada for an early HoLoccne Milankovitch thermal maximum. Nature, 305, 126-128,

Rodbell, D. T, Seltzer, G. G, Anderson, D. M,+ Abbott, M. B., Enfield, D. B., and Newman, J, H. (1999). An -"15,000-year record of El Niño - driven alUiviation in southwestern Ecuador. Science, 283,516-520.

Ruddiman, W. F, and Mix, A. C. (1993). The north and equatorial Atlantic al 9000 and 6000 yr BP. In Global Climates since the Last Glacial Maximum, eds. 11. E. Wright, Jr., J, E. kutzbach, T Webb, 111, W. E Ruddiman, F A, Street-Perrott,and P.J, Bartlein(Minneapolis, MN: University of Minnesota Press), 94-124.

Sandweiss, D., Richardson, J, IÍ., Rieitz, E, J., Rollins, H. FÍ,, and Maasch, K. A, (1996). Gcoar-chaelogical evidence from Peru for a 5000 years H P onset of El Niño. Science, 273, 1531-1533.

Schneider, S. í I., and Thompson, S-1 - (1979). Ice ages and orbital variations: some simple theory and modeling. Quat. Res., 12, 188-203.

Street-Perrott, F A., Mitchell, J. F. B,, Marc hand, D. S,, and Brunncr, J. S. (1990). Milankovitch and albedo forcing of the tropical monsoons: a comparison of geological ev idence and numerical simulations for 9000 yr HP. Transactions of the Royal Society of Edinburgh, 81, 407-427.

Street-Perrott, F. A., and Perrott, R. A, (1990), Abrupt climate fluctuations in the tropics: the influence of Atlantic Ocean circulation. Nature, 343, 607-612.

Suarez, M. J., and Held, I. M. (1976). Modeling climatic response to orbital parameter variations. Nature, 263,46 47,

TEMPO Members (1996), Potential role of vegetation feedback in the climaie sensitivity of high -latiiude regions: A case study at 6000 years 13.P. Glob. Biogeochem. Cve., 10(4}, 727-736.

1 exier, D., de Noblet, N., I iarrison, S. P., Haxeltine, A. Joussaume, S., Jolly, 1 >,, I .aarif, F, Prentice, L C, and Tarasov, P. (1997). Quantifying the role of biosphere-atmosphere feedbacks in climate change: a coupled model simulation for 6000 years BP and comparison with palaeodata for northern Eurasia and northern Africa. Clim. Dyn,, 13, 865-882.

Vavrus, S. J. (1999). The response of the coupled Arctic sea-icc atmosphere system to orbital forcing and ice motion at 6 kvr and 115 kyr BP. Jour, of Clim., 12, 873-8%.

Webb, T III, Burtlein, R J,, and Kui/bach, j, E, (1987), Climatic change in cistern North America during the past 18,(KH) years, comparisons of pollen data with model results. In The Geology of North Amenta: North Ameriem and adjacent oceans during the last deglaaation, K-3 447-462. Boulder, (X): Geological Society of America, Wright, H. EL, Jr. (1987). Synthesis: the land south of the ice sheets. In The Geology of North America: North America and adjacent oceans during the last degradation, K. 3 479—488, Moulder, CO: Geological Society of America. Wright, H. E., Jr., Kut/bach, j, E,, Webb, T 111, Ruddiman, W, F., Street-Perrutt, K A,, and llartlein, P. JL, eds. (1993), Global Climates since the Last Glacial Maximum (Minneapolis^ VtN: University of Minnesota Press), 569 pp.

0 0

Post a comment