Self-accelerated turbidity current prediction based upon (k-ɛ) turbulence
- 31 July 1989
- journal article
- Published by Elsevier in Continental Shelf Research
- Vol. 9 (7) , 617-627
- https://doi.org/10.1016/0278-4343(89)90033-2
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- Downslope Eulerian mean flow associated with high-frequency current fluctuations observed on the outer continental shelf and upper slope along the northeastern United States continental margin: implications for sediment transportContinental Shelf Research, 1988
- The scaling of turbulence in the presence of stable stratificationJournal of Geophysical Research: Oceans, 1988
- Application of theE– ϵ Turbulence Closure Model to the Neutral and Stable Atmospheric Boundary LayerJournal of the Atmospheric Sciences, 1988
- Experiments on turbidity currents over an erodible bedJournal of Hydraulic Research, 1987
- Oscillating turbulent boundary layer with suspended sedimentsJournal of Geophysical Research: Oceans, 1986
- Self-accelerating turbidity currentsJournal of Fluid Mechanics, 1986
- Sediment slides and turbidity currents on the Laurentian Fan: Sidescan sonar investigations near the epicenter of the 1929 Grand Banks earthquakeGeology, 1985
- Momentum Balance of Gravity FlowsJournal of the Atmospheric Sciences, 1982
- Interaction between velocity and effective density in turbidity flow: Phase-plane analysis, with criteria for autosuspensionMarine Geology, 1979
- A Sediment Transport Model for Straight Alluvial ChannelsHydrology Research, 1976