Response of low‐angle dunes to variable flow |
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| Authors: | Megan L Hendershot Jeremy G Venditti Ryan W Bradley Ray A Kostaschuk Michael Church Mead A Allison |
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| Affiliation: | 1. Department of Geography, Simon Fraser University, Burnaby, BC, Canada;2. Department of Geography, The University of British Columbia, Vancouver, BC, Canada;3. The Water Institute of the Gulf, Baton Rouge, LA, USA;4. Department of Earth & Environmental Sciences, Tulane University, New Orleans, LA, USA |
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| Abstract: | Current understanding of bedform dynamics is largely based on field and laboratory observations of bedforms in steady flow environments. There are relatively few investigations of bedforms in flows dominated by unsteadiness associated with rapidly changing flows or tides. As a consequence, the ability to predict bedform response to variable flow is rudimentary. Using high‐resolution multibeam bathymetric data, this study explores the dynamics of a dune field developed by tidally modulated, fluvially dominated flow in the Fraser River Estuary, British Columbia, Canada. The dunes were dominantly low lee angle features characteristic of large, deep river channels. Data were collected over a field ca 1·0 km long and 0·5 km wide through a complete diurnal tidal cycle during the rising limb of the hydrograph immediately prior to peak freshet, yielding the most comprehensive characterization of low‐angle dunes ever reported. The data show that bedform height and lee angle slope respond to variable flow by declining as the tide ebbs, then increasing as the tide rises and the flow velocities decrease. Bedform lengths do not appear to respond to the changes in velocity caused by the tides. Changes in the bedform height and lee angle have a counterclockwise hysteresis with mean flow velocity, indicating that changes in the bedform geometry lag changes in the flow. The data reveal that lee angle slope responds directly to suspended sediment concentration, supporting previous speculation that low‐angle dune morphology is maintained by erosion of the dune stoss and crest at high flow, and deposition of that material in the dune trough. |
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| Keywords: | Low‐angle dunes symmetrical dunes tidally influenced flows unsteady flow bedforms |
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