Scaling arguments

Recent CTD observations suggest local hydrography is variable on scales much smaller than expected vortex radius.

Turbulence at the source:

The flux Richardson number, Ri, allows comparison of the source fluxes of momentum and buoyancy. A Ri of one indicates equal contributions to the flow. Values less than one indicate jet-like behavior, while values greater than 1 correspond to plume-like behavior.

Source type:    Q         B         M         Ri
                cm/s      cm4/s3    cm4/s2   
---------------------------------------------------
350oC vents:    1.3x10^3  3.7x10^5  1.3x10^5  0.30
10oC  vents:    1.3x10^5  1.8x10^5  1.3x10^5  27
my source:      1.0       10^-2               very turbulent, orifice: 2mm     
H/B* source:    1.0                           wider orifice: 8mm 

Helfrich and Battisti report vortices with diameters of ~10cm at N/f~1.42. Their tank was square, and about 1.5 times as wide as mine...

Cross-flow is tough! How to get a tank big enough to have circumnavigation time >> rise time?

This suggests simplification. Try N=0 and no cross flow first...

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