Reproducing results of Helfrich and Battisti (1991):
(Plumes in rotating, stratified, quiescent fluid)

Helfrich and Battisti observed baroclinic vortices form at a central source
in stratified fluid, and then separate and migrate around their tank.
Initial stratification seemed pretty good, but adding fish flakes after the filling
was a big mistake. There was also a distinct, slow mean anticylonic flow in the tank.
The plume equilibrated at mid-depth, as hoped, and the circulation was definitely
anticyclonic, except very near the top of the tank, adjacent to the source.
A final experiment (trial 8) confirmed our basic intuition that these plumes
in this experimental set up should rotate anticyclonically at the outflow depth...

If you have comments, questions, or suggestions, email me at
scottv@ocean.washington.edu
This research was conducted within the
University of Washington Geophysical Fluid Dynamics Laboratory