Island Wakes in Deep Water

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Submesoscale currents in the ocean (2016, background): “Even in an idealized rotating, stratified simulation with unrealistic side walls, the lateral boundary layer and wake shear layers are quite thin when Re is large (or, more precisely, the horizontal Ekman number, Ekh = νh/f 2, is small), so the phenomenon can be viewed as usually within the submesos”
Submesoscale Instability and Generation of Mesoscale Anticyclones near a Separation of the California Undercurrent (2015, background): “Oceanic currents can also separate behind an island, headland, or submerged bump (e.g., Dong et al. 2007), as well as along a continuous coast because of the changing wind stress curl, boundary curvature away from the downstream flow direction, and an internally generated adverse pressure gradient…”