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March  2007, 7(2): 293-314. doi: 10.3934/dcdsb.2007.7.293

Is the subdominant part of the energy spectrum due to downscale energy cascade hidden in quasi-geostrophic turbulence?

Eleftherios Gkioulekas 1, and  Ka Kit Tung 2,

1. 

Department of Mathematics, University of Central Florida, Box 161364, Orlando, FL 32816-1364, United States
2. 

University of Washington, Department of Applied Mathematics, Box 352420, Seattle, WA 98195-2420

Received  August 2006 Revised  October 2006 Published  December 2006

In systems governing two-dimensional turbulence, surface quasi-geostrophic turbulence, (more generally $\alpha$-turbulence), two-layer quasi-geostrophic turbulence, etc., there often exist two conservative quadratic quantities, one "energy''-like and one "enstrophy''-like. In a finite inertial range there are in general two spectral fluxes, one associated with each conserved quantity. We derive here an inequality comparing the relative magnitudes of the "energy'' and "enstrophy'' fluxes for finite or infinitesimal dissipations, and for hyper or hypo viscosities. When this inequality is satisfied, as is the case of 2D turbulence,where the energy flux contribution to the energy spectrum is small, the subdominant part will be effectively hidden. In sQG turbulence, it is shown that the opposite is true: the downscale energy flux becomes the dominant contribution to the energy spectrum. A combination of these two behaviors appears to be the case in 2-layer QG turbulence, depending on the baroclinicity of the system.
Keywords: QG turbulence., 2d turbulence.
Mathematics Subject Classification: Primary: 76FXX; Secondary: 60G6.
Citation: Eleftherios Gkioulekas, Ka Kit Tung. Is the subdominant part of the energy spectrum due to downscale energy cascade hidden in quasi-geostrophic turbulence?. Discrete and Continuous Dynamical Systems - B, 2007, 7 (2) : 293-314. doi: 10.3934/dcdsb.2007.7.293
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