Double diffusive turbulence in sheared oceanic flow
William D. Smyth, Satoshi Kimura
College of Oceanic and Atmospheric Sciences, Oregon State University
This presentation describes the instability and turbulence that result when layers of sea water having different temperatures and salinities flow over one another. It is based on a presentation in preparation for the Supercomputing '07 conference in Reno, NV, November 2007.
