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Wind-invariant saltation heights imply linear scaling of aeolian saltation flux with shear stress
Wind-driven sand transport generates atmospheric dust, forms dunes, and sculpts landscapes. However, it remains unclear how the flux of particles in aeolian saltation—the wind-driven transport of sand in hopping trajectories—scales with wind speed, largely because models do not agree on how particle...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5462498/ https://www.ncbi.nlm.nih.gov/pubmed/28630907 http://dx.doi.org/10.1126/sciadv.1602569 |