Abstract. Almost fty years of investigations of barchan dunes morphology and dynamics is reviewed, with emphasis on the physical understanding of these objects. The characteristic quantities measured on the eld (shape, size, velocity) and the physical problems they rise are presented. Then, we review the dynamical mechanisms explaining the formation and the propagation of dunes. In particular a complete and original approach of the sand transport over a flat sand bed is proposed and discussed. We conclude on open problems by outlining future research directions. PACS. 45.70.-n Granular systems { 47.54.+r Pattern selection; pattern formation
[1] Barchans are propagating crescentic dunes that form in arid regions where strong, unidirectional...
International audience[1] We present a 1 year study of 50 dunes in a small field of barchan dunes in...
The present paper reports the formation of subaqueous barchan dunes by analyzing the temporal evolut...
Abstract. Almost fty years of investigations of barchan dunes morphology and dynamics is reviewed, w...
20 pages, 20 figuresAlmost fifty years of investigations of barchan dunes morphology and dynamics is...
Almost fifty years of investigations of barchan dunes morphology and dynamics is reviewed, with emp...
3 pages, 4 figuresWe demonstrate the feasibility of studying dunes in a laboratory experiment. It is...
[1] The structure of the barchan field located between Tarfaya and Laayoune (Atlantic Sahara, Morocc...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Lyderic Bocquet, Tomas Bohr, François Charru, Eric Clément et Francois MétivierBarchans are crescent...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Many complex aspects are involved in the morphodynamics of crescent-shaped dunes, known as barchans....
Aeolian sand dunes originate from wind flow and sand bed interactions. According to wind properties ...
[1] Barchans are propagating crescentic dunes that form in arid regions where strong, unidirectional...
International audience[1] We present a 1 year study of 50 dunes in a small field of barchan dunes in...
The present paper reports the formation of subaqueous barchan dunes by analyzing the temporal evolut...
Abstract. Almost fty years of investigations of barchan dunes morphology and dynamics is reviewed, w...
20 pages, 20 figuresAlmost fifty years of investigations of barchan dunes morphology and dynamics is...
Almost fifty years of investigations of barchan dunes morphology and dynamics is reviewed, with emp...
3 pages, 4 figuresWe demonstrate the feasibility of studying dunes in a laboratory experiment. It is...
[1] The structure of the barchan field located between Tarfaya and Laayoune (Atlantic Sahara, Morocc...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Lyderic Bocquet, Tomas Bohr, François Charru, Eric Clément et Francois MétivierBarchans are crescent...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Barchan dunes can be found in sand barren regions under steady wind conditions. They translate in th...
Many complex aspects are involved in the morphodynamics of crescent-shaped dunes, known as barchans....
Aeolian sand dunes originate from wind flow and sand bed interactions. According to wind properties ...
[1] Barchans are propagating crescentic dunes that form in arid regions where strong, unidirectional...
International audience[1] We present a 1 year study of 50 dunes in a small field of barchan dunes in...
The present paper reports the formation of subaqueous barchan dunes by analyzing the temporal evolut...