Fig. 7: Frequency spectra of velocity field in numerical experiments.
From: The hurricane-induced decay of mesoscale eddies: an energy source for near-inertial waves
a Spatially averaged power spectral density (PSD) for Case 1. b–f Same as a but for Cases 2–6. Dashed lines denote the Coriolis frequency f = 1 × 10−4 s−1.
