A bridge built inside the reversed flow region of a sand dune will change the characteristics of wind-sand movement in this region. The Reynolds-averaged Navier-Stokes simulation and discrete particle tracing are used to simulate the wind-sand movement around a sand dune with a bridge built inside the reversed region. Three cases with different bridge positions are studied. The results show that 1) compared with the isolated dune case, a tall bridge built at the leeward toe leads to an increase in the deposition rate on the leeward slope and a longer reversed flow region downstream of the sand dune; meanwhile, the high speed of crosswind on the bridge indicates that some measures should be taken to protect trains from strong crosswind; 2) a...
More than 4000 hourly wind profiles measured on three topographically different foredunes are analys...
The behaviour of offshore-directed winds over coastal dune and beach morphology was examined using a...
AbstractThe movements of sand dunes due to wind forces are studied by considering the boundary layer...
Conference Abstract: Aeolian sediment transport in desert and sandy coastal environments affects ci...
International audienceSand dune deformation is a dynamic process resulting from a complex interplay ...
This paper discusses the possibilities of laboratory simulation of large-scale flow around dunes, bo...
This study presents an analysis of wind flow and sediment transport from the beach, up a 50m high, l...
In the Netherlands, the coastal dunes are essential to protect the country against flooding. However...
This study presents an analysis of wind flow and sediment transport from the beach, up a 50m high, l...
Knowledge of wind flow over dune scarps and, as scarps fill, their subsequent various slopes, is imp...
Turbulent wind patterns over a two-dimensional isolated downsized barchan dune under the influence o...
Two kinds of Star dunes are simulated numerically in order to make clear the mechanism of their form...
Turbulent wind flow over hilly terrains has been extensively investigated in the scientific literatu...
Based on the test and observation of the desert hinterland wind field, combined with the numerical s...
After the construction of desert highway, the physiognomy changes caused by surface wind erosion and...
More than 4000 hourly wind profiles measured on three topographically different foredunes are analys...
The behaviour of offshore-directed winds over coastal dune and beach morphology was examined using a...
AbstractThe movements of sand dunes due to wind forces are studied by considering the boundary layer...
Conference Abstract: Aeolian sediment transport in desert and sandy coastal environments affects ci...
International audienceSand dune deformation is a dynamic process resulting from a complex interplay ...
This paper discusses the possibilities of laboratory simulation of large-scale flow around dunes, bo...
This study presents an analysis of wind flow and sediment transport from the beach, up a 50m high, l...
In the Netherlands, the coastal dunes are essential to protect the country against flooding. However...
This study presents an analysis of wind flow and sediment transport from the beach, up a 50m high, l...
Knowledge of wind flow over dune scarps and, as scarps fill, their subsequent various slopes, is imp...
Turbulent wind patterns over a two-dimensional isolated downsized barchan dune under the influence o...
Two kinds of Star dunes are simulated numerically in order to make clear the mechanism of their form...
Turbulent wind flow over hilly terrains has been extensively investigated in the scientific literatu...
Based on the test and observation of the desert hinterland wind field, combined with the numerical s...
After the construction of desert highway, the physiognomy changes caused by surface wind erosion and...
More than 4000 hourly wind profiles measured on three topographically different foredunes are analys...
The behaviour of offshore-directed winds over coastal dune and beach morphology was examined using a...
AbstractThe movements of sand dunes due to wind forces are studied by considering the boundary layer...