Horizontal shear instabilities in low-Froude high-Re stratified flows produce vertical shear through two distinct pathways, each leading to small-scale KH instabilities at large buoyancy Reynolds number but with different peak mixing efficiencies.
Proceedings of the Royal Society of London Series A , year = 1917, month = mar, volume =
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Two pathways to diapycnal mixing in strongly stratified flows with no initial vertical shear
Horizontal shear instabilities in low-Froude high-Re stratified flows produce vertical shear through two distinct pathways, each leading to small-scale KH instabilities at large buoyancy Reynolds number but with different peak mixing efficiencies.