How does the diffusion fish swim?

ORAL

Abstract

An asymmetric object (such as a wedge) placed in a stably stratified fluid moves with a steady horizontal speed. We explain how this spontaneous motion is caused by the diffusion-driven buoyancy layers that form on the sloping surfaces of the object, and calculate the speed for a variety of two-dimensional configurations using the method of matched asymptotic expansions. Surprisingly, in many cases, the leading-order speed depends on neither the viscosity nor the stratification strength.

*This work was completed at the 2015 WHOI GFD Program, which is supported by the National Science Foundation and the Office of Naval Research.

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Authors

  • Gunnar Peng

    • DAMTP, University of Cambridge

  • Neil Balmforth

    • Department of Mathematics, University of British Columbia
    • University of British Columbia

  • William Young

    • Scripps Institution of Oceanography
    • Scripps Institution of Oceanography, University of California at San Diego