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The mean circulation in a coastal zone of variable depth may under certain circumstances be modeled by linear equations, including a bottom friction linear in the depth-averaged velocity. The resultin...
Numerical Study of Topographic Wave Reflection in Semi-Infinite Channels
topographic wave reflections Semi-Infinite Channels Numerical Study
2009/1/5
The Potential vorticity equation describing topographic waves is approximately solved using the channel method of Stocker and Hutter. The domain of integration is a semi-infinite channel and models an...