Approximating Isoneutral Ocean Transport via the Temporal Residual Mean
Ocean volume and tracer transports are commonly computed on density surfaces because doing so approximates the semi-Lagrangian mean advective transport. The resulting density-averaged transport can be related approximately to Eulerian-averaged quantities via the Temporal Residual Mean (TRM), valid i...
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| Format: | Article |
| Language: | English |
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MDPI AG
2019-10-01
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| Series: | Fluids |
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| Online Access: | https://www.mdpi.com/2311-5521/4/4/179 |