Previous |  Up |  Next


[1] d’Almeida, G. A., Koepke, P., Shettle, E. P.: Atmospheric Aerosols — Global Climatology and Radiative Characteristics. A. Deepak Publishing, Hampton, Virginia 1991.
[2] d’Almeida, G. A.: A model for Saharan dust transport. Journal of Climatology and Applied Meteorology, Vol. 25 (1986), 903–916.
[3] Barnola, J. M., Raynaud, D., Korotkevich, Y. S., Lorius, C.: Vostok ice core provides 160,000-year record of atmospheric CO$_{2}$. Nature 329 (1987), 408–413.
[4] Berger, A., Fichefet, Th., Gallée, H., Tricot, Ch., Ypersele, J. P.: Entering the glaciation with a 2-D coupled climate model. Quaternary Science Reviews, Vol. 11 (1992), 481–493.
[5] Bohren, C. F., Huffman, D. R.: Absorption and Scattering of Light by Small Particles. John Wiley & Sons, New York, Chichester, Brisbane, Toronto, Singapore 1983.
[6] Businger, J. A., Wyngaard, J. C., Izumi, Y., Bradley, E. F.: Flux-profile relationships in the atmospheric surface layer. Journal of the Atmospheric Sciences, Vol. 28 (1971), 181–189.
[7] Duplessy, J. C., Labeyrie, L., Blanc, P. L.: Norwegian sea deep water variations over the last climatic cycle: Paleo-oceanographical implications. In: Long and Short Term Variability of Climate, Earth Sci. Ser., ed. H. Wanner, U. Siegenthaler, Springer-Verlag, New York 1988, pp. 83–116.
[8] Gallée, H., Ypersele, J. P. van, Fichefet, Th., Tricot, Ch., Berger, A.: Simulation of the last glacial cycle by a coupled, sectorially averaged climate–ice sheet model 1. The climate model. Journal of Geophysical Research, Vol. 96 (1991), 13.139–13.161.
[9] Gallée, H., Ypersele, J. P. van, Fichefet, Th., Marsiat, I., Tricot, Ch., Berger, A.: Simulation of the last glacial cycle by a coupled, sectorially averaged climate–ice sheet model 2. Response to insolation and CO$_{2}$ variations. Journal of Geophysical Research, Vol. 97 (1992), 15.713–15.740.
[10] Gillette, D. A.: Environmental factors affecting dust emission by wind erosion. In: Saharan Dust: Mobilization, Transport, Deposition (C. Morales ed.), SCOPE Rep. 14, John Wiley, New York 1979, 27–48.
[11] Hänel, G.: The properties of atmospheric aerosol particles as functions of the relative humidity at thermodynamic equillibrium with the sorrounding moist air. Advances in Geophysics, Vol. 19 (1976), 73–187.
[12] Haltiner, G. J., Williams, R. T.: Numerical Prediction and Dynamic Meteorology. Wiley and Sons (1980), 477 pp.
[13] Joussaume, S.: Three-dimensional simulations of the atmospheric cycle of desert dust particles using a general circulation model. Journal of Geophysical Research, Vol. 95 (1990), 1909–1941.
[14] Junge, C. E.: The importance of mineral dust as an atmospheric constituent. In: Saharan Dust, Mobilization, Transport and Deposition (C. Morales, ed.), John Wiley & Sons, Chichester, New York, Brisbane, Toronto 1979, 49–60.
[15] Kasahara, A.: Computational aspects of numerical models for weather prediction and climate simulation. In: Method in Computational Physics, 17 (1977), Academic Press, 2–66.
[16] Labeyrie, L. D., Duplessy, J. C., Blanc, P. L.: Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years. Nature, 327 (1987), 477-482.
[17] Nickling, W. G., Gillies, J. A.: Emission of fine-grained particulates from desert soils. In: Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport (M. Leinen and M. Sarnthein, eds.), NATO Adv. Study Inst. Ser., Ser. C, Vol. 282 (1989), Kluwer Academic, Dordecht, Netherlands, 133–165.
[18] Oort, A. H.: Global atmospheric circulation statistics 1958–1973, NOAA Prof. Pap. 14, NOAA, Washington, D. C. (1983), 180pp.
[19] Slinn, W. G. N.: Air-to-sea transfer of particles. In: Air-Sea Exchange of Gases and Particles (eds P. S. Liss and W. G. N. Slinn), NATO ASI Series, C 108, D. Reidel, Hingham, Mass. (1983), 299–405.
[20] Shackleton, N. J., Le, J., Mix, A., Hall, M. A.: Carbon isotope records from Pacific surface waters and atmospheric carbon dioxide. Quaternary Science Reviews 11 (1992), 387–400.
[21] Tegen, I., Fung, I.: Modelling of mineral dust in the atmosphere: Sources, transport and optical thickness. Journal of Geophys. Res. 99 (1994), 22,897–22,914.
[22] Toon, O. B., Turco, R. P., Westphal, D., Malone, R., Liu, M. S.: A multidimensional model for aerosols: Description of computational analogs. Journal of the Atmospheric Sciences, Vol. 45 (1988), 2123–2143.
[23] Westphal, D. L., Toon, O. B., Carlson, T. N.: A case study of mobilization and transport of Saharan dust. Journal of the Atmospheric Sciences, Vol. 45 (1988), 2145–2175.
[24] WCRP-112: A preliminary cloudless standard atmosphere for radiation computation. WCRP Report 112, WMO, Geneva 1986.
Partner of
EuDML logo