Balanced to Unbalanced Motions at a Submesoscale Front and Energy Transfer From Eddy Splitting
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research on submesoscale fronts and energy transfer is being reported, with studies examining the dynamics of these fronts in various oceanic contexts. the research appears to involve observations and simulations of submesoscale motions and their effects on energy transfer and oceanic processes. findings suggest that submesoscale fronts can induce vertical transport and are influenced by factors such as upper-ocean convergent flows and geostrophic strain.
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