Figure 5
From: Deep-sea Sediment Resuspension by Internal Solitary Waves in the Northern South China Sea
Velocity (E-W) for depth zones above 200 m measured using a hull-mounted ADCP: (a) T3 is located at 19°48′N,115°05′E at a depth of 1545 m and (b) T4 is located at 19°57′N, 115°18′E at a depth of 1252 m (Fig. 1). Red dashed square indicated the period included suspended sediment concentration and the mean velocity near the seabed in Fig. 4.
