Diminishing inverse transfer and non-cascading dynamics in surface quasi-geostrophic turbulence
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Publication:2492242
DOI10.1016/j.physd.2005.11.001zbMath1089.76024arXivnlin/0412025OpenAlexW2092520458MaRDI QIDQ2492242
Publication date: 9 June 2006
Published in: Physica D (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/nlin/0412025
Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Turbulent transport, mixing (76F25)
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Cites Work
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- The Eulerian limit for 2D statistical hydrodynamics
- Constraints on the spectral distribution of energy and enstrophy dissipation in forced two-dimensional turbulence
- A maximum principle applied to quasi-geostrophic equations
- A two-dimensional model for quasigeostrophic flow: Comparison with the two-dimensional Euler flow
- On the dual cascade in two-dimensional turbulence
- Extensivity of two-dimensional turbulence
- Nonlinear transfer and spectral distribution of energy in \(\alpha\) turbulence
- Spectra of local and nonlocal two-dimensional turbulence
- Exact results on stationary turbulence in 2D: Consequences of vorticity conservation
- On the critical dissipative quasi-geostrophic equation
- Nonlinear behavior and turbulence spectra of drift waves and Rossby waves
- Pseudo-three-dimensional turbulence in magnetized nonuniform plasma
- Formation of strong fronts in the 2-D quasigeostrophic thermal active scalar
- Large-scale energy spectra in surface quasi-geostrophic turbulence
- Turbulent diffusion in the geostrophic inverse cascade
- Singular front formation in a model for quasigeostrophic flow
- Effects of the forcing function spectrum on the energy spectrum in 2-D turbulence
- Surface quasi-geostrophic dynamics
- Diffusion Approximation for Turbulent Scalar Fields
- Computation of the Energy Spectrum in Homogeneous Two-Dimensional Turbulence
- Inertial-range transfer in two- and three-dimensional turbulence
- Inviscid and inviscid-limit behavior of a surface quasigeostrophic flow
