Fig. 2
From: Self-sharpening induces jet-like structure in seafloor gravity currents
Field site location and bathymetric maps. Field site location in the channelized gravity current system, SW Black Sea shelf (a). Inset shows geographical location. The density-driven exchange flow, driven by salinity differences between the Mediterranean and Black Sea22, has created a self-formed channelized network. Multi Beam Echo Sounder (MBES) bathymetry of the channel floor bedforms, (b), investigated here (see methods), where white dots denote the Autonomous Underwater Vehicle (AUV) tracks used in this study to obtain detailed flow velocity measurements, black arrows denote mean flow direction and black crosses denote conductivity-temperature-depth (CDT) cast locations
