Maps of baroclinic conversion of (a),(e) EKE (kg m 21 s 23 ), (b),(f)
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Topographic generation of submesoscale centrifugal instability and energy dissipation
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Maps of (a) baroclinic and (b) barotropic conversion rates averaged
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Bathymetry of the model domain. The contour interval is 100 m. The
Intensification of Pacific tropical instability waves over the recent three decades
OS - Constraining an eddy energy dissipation rate due to relative wind stress for use in energy budget-based eddy parameterisations
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Frontiers Seasonal variability of eddy kinetic energy in the north Indian Ocean
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