This is a good article for those interested in the dynamic in-stream interaction between flow and bed form, which is helpful for making sense of rating curve dynamics in steep mountain streams. “Channel state depends on local flow structure, supply of sediment, and forcing/boundary conditions, resulting in feedbacks between hydraulics, sediment transport, and bed topography.”

http://onlinelibrary.wiley.com/doi/10.1002/2017GL074198/full

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