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Jörn Callies and Raffaele Ferrari

-quasigeostrophic (QG) turbulence ( Blumen 1978 ) may be the relevant framework for interpreting the submesoscale turbulence that develops in response to frontogenesis. Fig . 2. Tracks along which measurements were collected in the (left) Oleander and (right) Spice experiments (thick black lines). The satellite tracks used in the analysis are shown as thin blue lines. The site of the mooring used for Fig. 1 is marked with a black dot. The background color is a map of eddy kinetic energy from the Archiving

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