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Shear, Strain, and Richardson Number Variations in the Thermocline. Part II: Modeling Mixing
Richardson Number Variations Thermocline Modeling Mixing
2008/11/12
Gregg has provided observational evidence that averaged estimates of dissipation, , vary approximately as the square of the internal wave field energy level E2. He notes that the finding is consiste...
Shear, Strain, and Richardson Number Variations in the Thermocline. Part I: Statistical Description
Surface Waves Processes Experiment isopycnal-following frames Thermocline
2008/11/12
Quasi-continuous depth–time observations of shear (5.5-m, 6-min resolution) and strain, (η/z, (2-m, 2.1- min resolution) obtained from the R/P FLIP are applied to a study of Richardson number (Ri) sta...