Flow dynamic

Wednesday, October 15, 2014 - 3:15pm - 4:05pm
Robert Weiss (Virginia Polytechnic Institute and State University)
Conventionally, two-dimensional and depth-averaged methods have been employed to
simulate the sediment deposition, transport and erosion in tsunamis and storms.
The simulations of the sediment dynamics for both events has the advantage that
we learn about the interaction of the respective flow and the movable bed in
general, but if done with consistent methods we can also learn about the
differences in sediment dynamics between tsunami and storms. The difference then
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