Cold filamentary intensification and oceanic surface convergence lines

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Submesoscale currents in the ocean (2016, background): “The central convergence in this secondary circulation provides an even more effective O(Ro) advective feedback in the buoyancy equation, hence a more rapid growth in ∂xb than in a front of comparable size and strength [47].”
Heat balance and eddies in the Peru-Chile current system (2012, background): “Lateral flux and vertical restratification are typical of eddy generation by baroclinic instability, as well as near-surface frontal and filamentary processes (Capet et al. 2008b; McWilliams et al. 2009a).”