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Summary and Conclusions
 
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- Breaking internal waves account for a significant portion of mixing and
dissipation within the world's oceans.
- Nonhydrostatic model is required to capture breaking internal wave physics.
- Unstructured grid is required for irregular domains.
- Parallelization is required to handle the problem size.
- Volume and mass conservation are guaranteed.
- Vertical advection/diffusion must be implicit when employing wetting and drying.
- Free-surface treatment must be implicit due to fast free-surface waves.
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20
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