Fig. 3: Current feedback results in a tidal imprint on the surface stress, air-sea energy flux and wind spectra.
From: Ocean tides can drag the atmosphere and cause tidal winds over broad continental shelves
Results from CTRL and NOCFB are shown for mid-Channel (red star in Fig. 2a): a Zonal current; b zonal surface stress; c co-spectrum (Λ) of the wind work. d 10 m zonal wind. In a, b, c, d a vertical line highlights the M2 tidal frequency.
