Wednesday, 25 January 2017: 11:00 AM
Conference Center: Chelan 2 (Washington State Convention Center )
In numerical computations of coastal circulation, a computational domain is truncated at locations aways from areas of interest and appropriate boundary conditions are prescribed at these locations. On the open ocean boundaries, it is important that a boundary treatment accurately introduce the desired information and minimize reflections of any outgoing waves. One of the most widely-used open-ocean boundary conditions simply forces a surface water level and is to a certain degree adequate for the former purpose. Unfortunately, this boundary condition is not a non-reflecting boundaries and could introduce detrimental effects. In this talk, we investigate the use of a sponge layer as a treatment for open-ocean boundaries in the context of (massively-parallel) continuous finite-element-based shallow water flow model. The sponge layer treatment yields a satisfactory results in a set of numerical tests and improve the robustness of the numerical model.
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