Abstract
Submarine fans, supplied primarily by turbidity currents, constitute the largest sediment accumulations on Earth. Generally accepted models of turbidity current behavior imply they should dissipate rapidly on the very small gradients of submarine fans, thus their persistence over long distances is enigmatic. We present numerical evidence, constrained by published field data, suggesting that turbidity currents traveling on low slopes and carrying fine particles have a stably stratified shear layer along their upper interface, which dramatically reduces dissipation and entrainment of ambient fluid, allowing the current to propagate over long distances. We propose gradient Richardson number as a useful criterion to discriminate between the different behaviors exhibited by turbidity currents on high and low slopes.
Original language | English |
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Pages (from-to) | 8608-8620 |
Number of pages | 13 |
Journal | Journal of Geophysical Research: Oceans |
Volume | 121 |
Issue number | 12 |
Early online date | 9 Dec 2016 |
DOIs | |
Publication status | Published - Dec 2016 |
Keywords
- turbidity current
- sediment transport
- stable stratification