Internal solitary waves in a structured thermocline with implications for resuspension and the formation of thin particle‐laden layers
- 15 May 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 106 (C5), 9565-9585
- https://doi.org/10.1029/2000jc900101
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- A mechanism for sediment resuspension by internal solitary wavesGeophysical Research Letters, 1999
- On the equation for spherical-particle motion: effect of Reynolds and acceleration numbersJournal of Fluid Mechanics, 1998
- Localized mixing due to a breaking internal wave ray at a sloping bottomJournal of Fluid Mechanics, 1997
- Particle transport by nonbreaking, solitary internal wavesJournal of Geophysical Research: Oceans, 1997
- Near‐boundary mixing above the flanks of a midlatitude seamountJournal of Geophysical Research: Oceans, 1997
- A Simple Model for the Shear-induced Decay of an Internal Solitary WaveJournal of Physical Oceanography, 1993
- Predictable Upwelling and the Shoreward Transport of Planktonic Larvae by Internal Tidal BoresScience, 1991
- The variability of mixing at the continental slopePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1990
- Vertical mixing due to the breaking of critical internal waves on sloping boundariesJournal of Fluid Mechanics, 1989
- Equation of motion for a small rigid sphere in a nonuniform flowPhysics of Fluids, 1983