|
|
|
|
|
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...
ver más
|
|
|
|
|
|
|
|
|
|
|
Markus Foerst and Nils Rüther
In recent years, advanced methods for measuring riverbank migration have been used to understand the process of river planform evolution. However, the role of the so-called outer secondary cell in the hydraulic pattern in bank erosion remains unclear. Fo...
ver más
|
|
|
|
|
|
|
|
|
|
|
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...
ver más
|
|
|
|
|
|
|
|
|
|
|
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...
ver más
|
|
|
|
|
|