Extended Data Fig. 1: Evidence for tidal signal and sediment re-suspension within Tungue Canyon at mooring C05A.
From: Highly variable deep-sea currents over tidal and seasonal timescales
a, Rose diagram showing the speed and direction for each measurement from the current metre located 3 mAB with data points coloured the corresponding ADCP acoustic backscatter measurement recorded at 15 mAB (that is the most bed proximal measurement). b, Power spectral density based on current direction measurements to show M2, semi-diurnal (12.4 h), and M4 (6.2 h) tidal constituents.
