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Three dimensional dunes of crescentic shape, called barchans, are commonly found on Earth and other planetary environments. In the great majority of cases, barchans are organized in large fields in which corridors of size-selected barchans…

Barchan dunes, or simply barchans, are crescent-shaped dunes found in diverse environments such as the bottom of rivers, Earth's deserts and the surface of Mars. In a recent paper [Phys. Rev. E 101, 012905 (2020)], we investigated the…

Geophysics · Physics 2021-01-26 Carlos Azael Alvarez Zambrano , Erick de Moraes Franklin

Crescentic shape dunes, known as barchan dunes, are formed by the action of a fluid flow on a granular bed. These bedforms are common in many environments, existing under water or in air, and being formed from grains organized in different…

Soft Condensed Matter · Physics 2018-10-29 Erick M. Franklin , Carlos A. Alvarez

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. In the case of subaqueous…

Fluid Dynamics · Physics 2019-10-11 Carlos Azael Alvarez , Erick de Moraes Franklin

Barchans are eolian dunes of crescent shape found on Earth, Mars and other celestial bodies. Among the different types of barchan-barchan interaction, there is one, known as chasing, in which the dunes remain close but without touching each…

Corridors of size-selected crescent-shaped dunes, known as barchans, are commonly found in water, air, and other planetary environments. The growth of barchans results from the interplay between a fluid flow and a granular bed, but their…

Geophysics · Physics 2021-08-24 Willian Righi Assis , Erick de Moraes Franklin

Barchans are crescent-shaped dunes commonly found in diverse environments and scales: from the 10-cm-long barchans found under water to the 1-km-long barchans on Mars, passing by the 100-m-long dunes on Earth's deserts. Although ubiquitous…

In the realm of granular bedforms, barchan dunes are strong attractors that can be found in rivers, terrestrial deserts and other planetary environments. These bedforms are characterized by a crescentic shape, which, although robust,…

Fluid Dynamics · Physics 2020-01-29 Carlos Azael Alvarez Zambrano , Erick de Moraes Franklin

Barchans are crescentic dunes propagating on a solid ground. They form dune fields in the shape of elongated corridors in which the size and spacing between dunes are rather well selected. We show that even very realistic models for…

Condensed Matter · Physics 2009-11-10 P. Hersen , K. H. Andersen , H. Elbelrhiti , B. Andreotti , P. Claudin , S. Douady

Barchans are dunes of high mobility which have a crescent shape and propagate under conditions of unidirectional wind. However, sand dunes only appear above a critical size, which scales with the saturation distance of the sand flux [P.…

Other Condensed Matter · Physics 2007-05-23 Eric J. R. Parteli , Orencio Duran , Hans J. Herrmann

We investigate the behavior of subaqueous barchans reaching dune-size obstacles by carrying out experiments where we varied the obstacle shape and size, the flow strength, and the grains' properties. We found that a subaqueous barchan can…

We investigate experimentally the short-range interactions occurring between two subaqueous barchans. The experiments were conducted in a water channel of transparent material where controlled grains were poured inside, and a camera placed…

Geophysics · Physics 2020-09-29 Willian Righi Assis , Erick de Moraes Franklin

Barchans are isolated mobile dunes often organized in large dune fields. Dune fields seem to present a characteristic dune size and spacing, which suggests a cooperative behavior based on dune interaction. In Duran et al. (2009), we propose…

Soft Condensed Matter · Physics 2011-05-20 Orencio Durán , Veit Schwämmle , Pedro G. Lind , Hans J. Herrmann

We inquire into the morphodynamics of barchans under seasonal flows. For that, we carried out grain-scale numerical computations of a subaqueous barchan exposed to two-directional flows, and we varied the angle and frequency of…

Sand dunes are ubiquitous in nature, and are found in abundance on Earth and other planetary environments. One of the most common types are crescent-shaped dunes known as barchans, whose mid-line could be assumed to behave as 2D dunes. In…

Geophysics · Physics 2025-05-13 Willian Righi Assis , Erick de Moraes Franklin , Nathalie Vriend

Barchans are crescent-shaped sand dunes forming in aride regions with unidirectional wind and limited sand supply. We report analytical and numerical results for dune shapes under different environmental conditions as obtained from the…

Soft Condensed Matter · Physics 2009-11-11 Klaus Kroy , Sebastian Fischer , Benedikt Obermayer

Barchans are dunes commonly found in dune fields on Earth, Mars and other celestial bodies, where they can interact with each other. This article concerns experimental data for the flow over subaqueous barchans that are either isolated or…

Fluid Dynamics · Physics 2024-01-09 Jimmy Gabriel Alvarez , Danilo da Silva Borges , Erick de Moraes Franklin

Barchans are crescent-shape dunes ubiquitous on Earth and other celestial bodies, which are organized in barchan fields where they interact with each other. Over the last decades, satellite images have been largely employed to detect…

Beautiful dune patterns can be found in deserts and along coasts due to the instability of a plain sheet of sand under the action of the wind. Barchan dunes are highly mobile aeolian dunes found in areas of low sand availability and…

Other Condensed Matter · Physics 2009-11-10 O. Duran , V. Schwaemmle , H. Herrmann

Barchan dunes --- crescent-shaped dunes that form in areas of unidirectional winds and low sand availability --- commonly display an asymmetric shape, with one limb extended downwind. Several factors have been identified as potential causes…

Soft Condensed Matter · Physics 2013-12-03 Eric J. R. Parteli , Orencio Durán , Mary C. Bourke , Haim Tsoar , Thorsten Poeschel , Hans J. Herrmann
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