Abstract
An important dynamical question involves how oceanic balanced flows lose energy. Recent numerical and analytical studies suggest topography catalyzes energy exchanges between balanced flows and a variety of unbalanced phenomena, which presumably leads to dissipation. We here develop a general theory of inviscid balanced flow interactions with walls that predicts submesoscale and unbalanced flow generation. Comparison with primitive equation-based numerical experiments supports the basic tenets of the theory.
Original language | English |
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Pages (from-to) | 501-522 |
Number of pages | 22 |
Journal | Journal of Marine Research |
Volume | 69 |
Issue number | 4-6 |
DOIs | |
Publication status | Published - Jul 2011 |