The energetic isotropic turbulence generated by a waterfall of low head was found to be developed in part through the unstable two-phase flow of entrained air bubbles. The resulting turbulent field had a turbulent Reynolds number of ≳2×104 and maintained a self-similar structure throughout the decay period studied. The present study may provide some insight into the structure of turbulence produced by the breaking waves over the ocean.
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Ling et al. (1977) studied this question.
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