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Barchan dunes are bed forms found in many sedimentary environments with a limited supply of sediment, and may occur in isolation or in more complex dune fields. Barchans have a crescentic planform morphology with horns elongated in the flow direction. To study flow over barchan dunes, we performed large eddy simulations in a channel with different interdune spacings.
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This page is a summary of: Large eddy simulation of interacting barchan dunes in a steady, unidirectional flow, Journal of Geophysical Research Earth Surface, October 2013, American Geophysical Union (AGU),
DOI: 10.1002/jgrf.20149.
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