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effect. A three-dimensional numerical simulation of wind around Imja definitely shows the upwind topographic screening effect. The hydrodynamics of Tsho Rolpa was simulated by creating a three-dimensional lake basin of actual size in the calculation domain. In the simulation, a return current, activated by the inflow-outflow system of the lake, was observed. Spatial distributions of the concentration and size for suspended sediment were also simulated, which was reasonable in pattern to the observation.
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