Generation of internal undular bores by transcritical flow over topography
In both the ocean and the atmosphere, the interaction of a density stratified flow with topography can generate large-amplitude, horizontally propagating internal solitary waves. Often these waves appear as a wave-train, or undular bore. In this article we focus on the situation when the flow is cri...
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| Main Authors: | , , |
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| Format: | Default Preprint |
| Published: |
2006
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| Subjects: | |
| Online Access: | https://hdl.handle.net/2134/719 |
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