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The Role of a Finite Density Jump at the Bottom of the Quasi-Continuous Ventilated Thermocline
Finite Density Jump Quasi-Continuous Ventilated Thermocline
2008/6/30
The ocean thermocline is resolved in a very large number of layers by means of a recursive relation that extends the LPS model of the ventilated flow from a small to an arbitrary number of layers. In ...