Physics of desertification edited by F. El-Baz, M.H.A. Hassan.
Deserts are parts of the Earth that receive little or no rain; 25 cm or less per year. The physical processes that act upon these parched lands are vastly different from those that shape the more humid parts of the terrestrial landmasses. In the desert, wind is a major agent of erosion and transport...
Full description
Saved in: