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Karen Garcia Angulo and Kwan Tun Lee
The Upper Amazon River forms an anabranching planform, which has been found to have significant changes in migration rate and river morphology. Previous studies have elaborated long-term evolution of the anabranching systems; however, research on the inf...
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Lukas Vonwiller, David F. Vetsch and Robert M. Boes
Sediment replenishment by artificial gravel deposits is a measure to increase sediment supply in gravel-bed rivers. Thereby, streambank erosion is the dominant process for gravel entrainment. In this contribution, we quantitatively validate a numerical m...
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Celso F. Castro-Bolinaga and Garey A. Fox
The special issue ?Streambank Erosion: Monitoring, Modeling, and Management? presents recent progress and outlines new research directions through the compilation of 14 research articles that cover topics relevant to the monitoring, modeling, and managem...
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Waldemar Kociuba and Grzegorz Janicki
Lower parts of proglacial rivers are commonly assumed to be characterised by a multiannual aggradation trend, and streambank erosion is considered to occur rarely and locally. In the years 2009?2013, detailed measurements of channel processes were perfor...
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Badal Mahalder, John S. Schwartz, Angelica M. Palomino and Jon Zirkle
The jet test device has been predominantly used for in situ critical shear stress (tc) and erodibility coefficient (kd) measurements of cohesive streambanks/beds using three analytical procedures: the Blaisdell method (BM), the iterative approach (IP), a...
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Siavash Hoomehr, Akinrotimi I. Akinola, Theresa Wynn-Thompson, Waverly Garnand and Matthew J. Eick
Increasing human populations and global climate change will severely stress our water resources. One potential unforeseen consequence of these stressors is accelerated stream channel erosion due to increased stream temperatures and changes in stream chem...
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William Beck, Thomas Isenhart, Peter Moore, Keith Schilling, Richard Schultz and Mark Tomer
Streambank erosion may represent a significant source of sediment and phosphorus (P) to overall watershed loads; however, watershed-scale quantification of contributions is rare. In addition, streambanks are often comprised of highly variable stratigraph...
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Da Liu, Manousos Valyrakis and Richard Williams
Riverbank vegetation is of high importance both for preserving the form (morphology) and function (ecology) of natural river systems. Revegetation of riverbanks is commonly used as a means of stream rehabilitation and management of bank instability and e...
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Holly K. Enlow, Garey A. Fox and Lucie Guertault
Two fluvial erosion models are commonly used to simulate the erosion rate of cohesive soils: the empirical excess shear stress model and the mechanistic Wilson model. Both models include two soil parameters, the critical shear stress (tc) and the erodibi...
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