Distinguishes between the forms of pure accumulations of barchan structures, transverse chains, linear dunes and star dunes; and erosional forms of parabolic dunes, and sandridges. These two classes appear to be responses to different sediment budgets. The excessive budget results from a wind saturated with sand and is responsible for the ergs of transverse chains. The deficient budget is due to a change in climate. Includes a review of climatic control mechanisms which apply to each of these aeolian structures.-from Author
CITATION STYLE
Mainguet, M. (1984). A classification of dunes based on aeolian dynamics and the sand budget. Deserts and Arid Lands, 31–58. https://doi.org/10.1007/978-94-009-6080-0_2
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