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Diapycnal fluxes of momentum and heat produced by three‐dimensional turbulence play important, but poorly understood, roles in the dynamics of the main thermocline and of the equatorial undercurrent. Diverse approaches—involving inferences, measurements, and process studies—are being pursued to define these fluxes and their significance. These are reviewed to improve the coordination of future mixing studies.
Michael C. Gregg (Fri,) studied this question.
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