Figure 2
From: Diurnal and semidiurnal internal waves on the southern slope of the Yermak Plateau
Rotary frequency spectra of horizontal baroclinic velocities at the three moorings (shading, unit: m2/s2/cpd). CW and CCW components are shown in (a–c) and (d–f), respectively. Tidal frequencies are indicated by black dashed lines, while local inertial frequency by red dashed lines.
