On a wave‐induced turbulence and a wave‐mixed upper ocean layer

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Wind Waves in the Coupled Climate System (2012, background): “—, A. Ganopolski, and W. R. C. Phillips, 2009: Waveinduced upper-ocean mixing in a climate model of intermediate complexity.”
On the Existence of Water Turbulence Induced by Nonbreaking Surface Waves (2009, background): “This is close to the lower-margin estimate of the critical Reynolds number of Babanin (2006).”
Evolution of the global wind wave climate in CMIP5 experiments (2012, background): “Wind and wind waves are key factors that have strong impacts on the exchange of energy and momentum between the atmosphere and the ocean [Donelan et al., 1997] and influence the mixing of upper ocean [Babanin, 2006; Babanin et al., 2009; Pleskachevsky et al., 2011; Qiao and Huang, 2012].”
Observation-Consistent Input and Whitecapping Dissipation in a Model for Wind-Generated Surface Waves: Description and Simple Calculations (2012, background): “Another theorized mode of energy loss is from turbulence generated by the nonbreaking orbital motion of waves (Babanin 2006).”
Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, background): “emperature in long-term coupled climate integrations. This latter mixing process appears similar to the mixing due to the high Reynolds numbers of the orbital motion of non-breaking waves explored by Babanin (2006) and Babanin and Haus (2009). Using a climate model of intermediate complexity, Babani”