Laboratory and numerical studies of internal wave generation and propagation in the ocean
Internal waves are generated in the ocean by oscillating tidal flow over bottom topography such as ridges, seamounts, and continental slopes. They are similar to the more familiar surface waves, but not being constrained to move on the surface, propagate throughout the bulk of the world oceans. Inte...
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Format: | Others |
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2014
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Online Access: | http://hdl.handle.net/2152/23459 |