Submesoscale Instability and Generation of Mesoscale Anticyclones near a Separation of the California Undercurrent

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Submesoscale currents in the ocean (2016, methodology): “This causes a dilution of the core ζ and qE anomalies to subcritical values by mixing, the formation of interior coherent vortices, and subsequent flow organization into another type of long-lived SCV, Cuddies (California Undercurrent eddies).”