Observations of the velocity profile of a fast and deep oceanic density current constrained in a gully

The southwestern side of the Wyville Thomson Ridge transports cold Faroe‐Shetland Channel Bottom Water in a narrow cascade from a depth of 500 m down to 1700 m. An upward looking acoustic Doppler current profiler located at a depth of 1200 m measured its currents to a height of 500 m for 6 months. T...

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