Thursday, 16 June 2005
Thomas Paine B (Hyatt Regency Cambridge, MA)
Although the hydrostatic approximation underlies much of theoretical geophysical fluid dynamics, aspect ratio effects have rarely been examined directly. In this work we consider aspect ratio effects in the context of an idealised problem: decaying, homogeneous turbulence.
Starting from previous work on the three-dimensionalization of decaying 2-D turbulence, we show that the aspect ratio strongly affects the saturation level of the perturbation and its feedback on the base flow. The saturation level scales linearly with the aspect ratio, as does the total damping exerted by the perturbation. A surprising result is the persistence of coherent vortices even after the saturation of the perturbation. The return to isotropy is slow.
Reference: K. Ngan, D.N. Straub and P. Bartello, ``Three-dimensionalization of freely-decaying two-dimensional turbulence,'' Phys. Fluids (16), 2918 (2004).
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