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Internal tide energy flux over a ridge measured by a co-located ocean glider and moored acoustic Doppler current profiler

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Figure

Figure 1. (a) Location of the experiment site (white square) and regional bathymetry, including the Faroe Bank Channel (FBC), Faroe–Shetland Channel (FSC), and Wyville Thomson Ridge (WTR)
Figure 2. (a) Absolute Salinity (colour) and Conservative Temperature (black contours, interval: 1velocities are northeast (down-slope)
Figure 3. (a) Across-slope barotropic velocity (black), the D2 component (grey), and a D2 harmonic fit to DAC velocity (magenta).(c) Across-slope baroclinic velocity (colour) overlaid with potential density (black contours, interval: 0.1 kg m−3)
Figure 3 shows potential density (Fig. 3c and d) and the D2component of vertical isopycnal displacement (Fig
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