In a global ocean simulation, pair dispersion is controlled by slow, balanced currents even when internal waves dominate the small-scale kinetic energy spectrum.
K., 1950: The application of the similarity theory of turbulence to atmospheric diffusion
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Effects of high-frequency and balanced motions on Lagrangian pair dispersion at the ocean surface
In a global ocean simulation, pair dispersion is controlled by slow, balanced currents even when internal waves dominate the small-scale kinetic energy spectrum.