Reach scale variability of turbulent flow characteristics in a gravel-bed river
In gravel-bed rivers, bed roughness is often controlled by the spatial distribution of pebble clusters and large protuberant clasts. The turbulent flow structure around these roughness elements has been studied extensively as opposed to the effects of the spatial variability of the bed roughness on...
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Veröffentlicht in: | Geomorphology (Amsterdam) 2005-05, Vol.68 (1), p.95-113 |
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Format: | Artikel |
Sprache: | eng |
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