From Macro- to Microscale: A combined modelling approach for near-surface wind flow on Mars at sub-dune length-scales. [PDF]
Love R +5 more
europepmc +1 more source
Th e sources of moisture in the barchans of Western Sahara
The aim of the study was to determine the impact of climatic and meteorological conditions on aeolian sand transport within barchans. The study area was located at Western Sahara, around the towns of Tarfaya and Laâyoune. Particular attention was paid to
Dluzewski, M. +3 more
core
Mean sediment residence time in barchan dunes
International audienceWhen a barchan dune migrates, the sediment trapped on its lee side is later mobilized when exposed on the stoss side. Then sand grains may undergo many dune turnover cycles before their ejection along the horns, but the amount of ...
Zhang, D. +3 more
core +1 more source
Widespread Megaripple Activity Across the North Polar Ergs of Mars. [PDF]
Chojnacki M +3 more
europepmc +1 more source
The Initial Opening of the Drake Passage Occurred During ca. 62‐59 Ma
Although the Drake Passage has been considered a critical component of ocean circulation and climate, its initial opening age remains controversial due to the weak constraints on the paleoposition of the Antarctic Peninsula.
Liang Gao +16 more
doaj +1 more source
Horns of subaqueous barchan dunes : a study at the grain scale
Many complex aspects are involved in the morphodynamics of crescent-shaped dunes, known as barchans. One of them concerns the trajectories of individual grains over the dune and how they affect its shape.
Alvarez, Carlos A., Franklin, Erick M.
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Equilibrium versus disequilibrium of barchan dunes
Barchans are crescent dunes which take place in mainly mono-directional winds. Shape, aspect ratios and velocities of these dunes had been studied as if they were in equilibrium, in a stable state.
EL BELRHITI Hicham, DOUADY Stéphane
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Shape evolution of numerically obtained subaqueous barchan dunes
In the realm of granular bedforms, barchan dunes are strong attractors that can be found in rivers, terrestrial deserts, and other planetary environments.
Alvarez, Carlos A., Franklin, Erick M.
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Strong-wind events control barchan dune migration
Wind is the most important external force in shaping aeolian landforms. Yet, it remains unclear what role the strong-wind events will play in the development of aeolian landforms compared with the effect of regular winds.
Hongjing Ren +5 more
doaj +1 more source
Geochemical, Mineralogical, and Geomorphological Characterization of Ash Materials as a Tracer for the Origin of Shifting Sands near Oldupai Gorge, Ngorongoro, Tanzania. [PDF]
Makongoro MZ +3 more
europepmc +1 more source

