Resarch Interests
* Stratified turbulence
* Spurious numerical mixing
* Horizontal Convection
* Effect of topography in overflows
* Performance of 2nd order turbulence closures in OGCMs
* Hydraulically controlled flows in narrow straits
Fig. Evolution of the passive tracer isosurface field in an overflow passing over a ridge. The dense isosurface (red) mixes and disappears when it passes over the ridge.