Vertical flow in the Southern Ocean estimated from individual moorings
In this study, we demonstrate that oceanic vertical velocities can be estimated from individual mooring measurements, even for non-stationary flow. This result is obtained under three assumptions: i. weak diffusion (Péclet number ?1), ii. weak friction (Reynolds number ?1), and iii. small inertial...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2015-09.
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| Subjects: | |
| Online Access: | Get fulltext |