Gravity currents in cold fresh water.
We consider surface gravity currents in fresh water where the temperatures of the current and the ambient are on opposite sides of the temperature of maximum density. Buoyancy reversal may occur in the current, due to entrainment of ambient water to produce a mixture that is denser than the ambient....
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| Format: | Default Preprint |
| Published: |
2005
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| Online Access: | https://hdl.handle.net/2134/568 |
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