4.7 Article

Swept away by a turbidity current in Mendocino submarine canyon, California

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 21, Pages 7611-7618

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL061863

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Funding

  1. David and Lucile Packard Foundation

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We present unique observations and measurements of a dilute turbidity current made with a remotely operated vehicle in 400 m water depth near the head of Mendocino Canyon, California. The flow had a two-layer structure with a thin (0.5 to 30 m), relatively dense (<0.04 vol %) and fast (up to similar to 1.7 m/s) wedge-shaped lower layer overlain by a thicker (up to 89 m) more dilute and slower current. The fast moving lower layer lagged the slow moving, dilute flow front by 14 min, which we infer resulted from the interaction of two initial pulses. The two layers were strongly coupled, and the sharp interface between the layers was characterized by a wave-like instability. This is the first field-scale data from a turbidity current to show (i) the complex dynamics of the head of a turbidity current and (ii) the presence of multiple layers within the same event.

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