1. Andreae, M. O., “Climatic effects of changing atmospheric aerosol levels,” in World Survey of Climatology, 16, Future climates of the world, A. Henderson-Sellers, Ed., Elsevier, Amsterdam, 347–398, 1995.
2. Bagnold, R.A., The Physics of Blown Sand and Desert Dunes, Mehuen, London, 265 pp., 1941.
3. Chepil, W.S., Properties of soil which influrence wind erosion, 4: State of dry aggregate structure, Soil Sci., 72, 387–401, 1951.
4. Chiapello I. and C. Moulin, TOMS and METEOSAT satellite records of the variability of Saharan dust transport over the Atlantic during the last two decades (1979–1997), Geophys. Res. Lett., 29, 17–20, 2002.
5. Dentener, F. J., G. R. Carmichael, Y. Zhang, J. Lelieveld, and P. Crutzen, Role of mineral aerosol as a reactive surface in the global troposphere, J. Geophys. Res., 101, 22, 869–22, 889, 1996.