Andreotti, B., Fourrière, A., Ould-Kaddour, F., Murray, B. and Claudin, P.2009: Giant aeolian dune size determined by the average depth of the atmospheric boundary layer. Nature457, 1120-23.
2.
Corbel, J.1959: Vitesse d’érosion. Zeitschrift f ür Geomorphologie NF3, 1-28.
3.
Lancaster, N., Kocurek, G., Singhvi, A., Pandey, V., Deynoux, M., Ghienne, J.-F. and Lô, K.2002: Late Pleistocene and Holocene dune activity and wind regimes in the western Sahara Desert of Mauritania. Geology30, 991-94.
4.
Mainguet, M. and Chemin, M.-C.1983: Sand seas of the Sahara and Sahel: an explanation of their thickness and sand dune type by the sand budget principle. In Brookfield, M.E. and Ahlbrandt, T.S., editors, Eolian sediments and landforms, Developments in Sedimentology 38, Amsterdam: Elsevier, 353-63.
5.
Petrov, M.P.1973: The deserts of the world (in Russian). Leningrad: Nauka, 435 pp. (Translated into English and published by Wiley in 1976.).
6.
Swezey, C.S.2009: Cenozoic stratigraphy of the Sahara, Northern Africa. Journal of African Earth Sciences53, 89-121.
7.
Wilson, I.G.1970: The external morphology of wind-laid sand deposits. Doctoral thesis, University of Reading, 181 pp.
8.
Wilson, I.G.1971: Journey across the Grand Erg Oriental. The Geographical Magazine43(4), 264-70.
9.
Wilson, I.G.1972a: Sand waves. New Scientist53(788), 634-37.
10.
Wilson, I.G.1972b: Aeolian bedforms - their development and origin. Sedimentology19, 173-210.
11.
Wilson, I.G.1972c: Universal discontinuities in bedforms produced by the wind. Journal of Sedimentary Petrology42, 667-69.