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Titlebook: River Dynamics and Integrated River Management; Zhao-Yin Wang,Joseph H. W. Lee,Charles S. Melching Book 2015 Tsinghua University Press, Be

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Integrated River Management,sented. In alluvial rivers, the average velocity increases with an increase in discharge when the discharge is small. As the discharge exceeds the bank-full discharge, any further increase in discharge does not result in an increase in velocity. The average velocity approaches a limit, which is the
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Tsinghua University Press, Beijing and Springer-Verlag Berlin Heidelberg 2015
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https://doi.org/10.1007/978-3-642-25652-3Geomorphology; Hydraulic Engineering; Stream Ecology; TUP
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Vegetation-Erosion Dynamics,water erosion, wind erosion, gravity erosion, glacier erosion and cultural erosion. Water erosion occurs in different forms: splash erosion, sheet erosion, rill erosion, gully erosion and channel erosion. Grain erosion is defined as the phenomenon of breaking down of bare rocks under the action of s
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