Titlebook: River, Coastal and Estuarine Morphodynamics; Giovanni Seminara,Paolo Blondeaux Book 2001 Springer-Verlag Berlin Heidelberg 2001 Entrainmen

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Alluvial Roughness in Streams with Dunes: A Boundary-Layer Approach,chers involved in a variety of problems including river hydraulics and other geophysical and environmental flows. Resistance to flow in alluvial streams has been widely investigated. Since the pioneer work of Exner [12] and, later, Einstein and Barbarossa [8], the profound effects of movable sedimen

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The Use of Numerical Models in Coastal Hydrodynamics and Morphology,to erosion or sedimentation, the flow pattern changes correspondingly. This means that a theoretical study of the morphological development of a specific case usually requires not only one flow calculation, but a large number of calculations.

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Process of Occurrence, Flow and Deposition of Viscous Debris Flow,erstitial water to behave as a kind of fluid. When the fine fraction is composed of cohesive solids and it accounts for a significant ratio in the entire particle fractions, the interstitial fluid becomes highly viscous slurry. In addition to the large viscosity of the slurry, the dense content of c

capillaries

Transverse Slope of Bed and Turbid-Clear Water Interface of Channelized Turbidity Currents Flowing held in suspension. These currents are capable of creating highly meandering channels extending over hundreds or thousands of kilometers. The planforms of these channels show a remarkable resemblance to those of meandering rivers. In order to understand the flow of turbidity currents in sinuous chan

employor

Pattern Formation in the Nearshore,m centimeters to kilometers. Since the bathymetry acts as a boundary condition to the progressing waves and those waves also slowly modify the bathymetry, an important feedback loop exists. It appears to be this feedback that causes observed nearshore morphologies, rather than the sand simply respon

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River and Tidal Networks,a tidal network, relies on accurate digital mapping technologies and on objective manipulations of remotely sensed imaging. Such analyses reveal extraordinary diversity of natural forms, and yet deep regularity and symmetry, regardless of a variety of environmental factors — what strikes is diversit

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