2012
DOI: 10.1103/physreve.86.066308
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Wave-number–frequency spectrum for turbulence from a random sweeping hypothesis with mean flow

Abstract: We derive the energy spectrum in wave-number-frequency space for turbulent flows based on Kraichnan's idealized random sweeping hypothesis with additional mean flow, which yields the instantaneous energy spectrum multiplied by a Gaussian frequency distribution. The model spectrum has two adjustable parameters, the mean flow velocity and the sweeping velocity, and has the property that the power-law index of the wave-number spectrum translates to the frequency spectrum, invariant for arbitrary choices of the me… Show more

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Cited by 70 publications
(95 citation statements)
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“…Furthermore, the spectral index is the same both in the frequency domain and in the wavenumber domain (Wilczek and Narita, 2012). The effect of the sweeping velocity appears in the coefficient of the frequency spectrum.…”
Section: Discussionmentioning
confidence: 78%
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“…Furthermore, the spectral index is the same both in the frequency domain and in the wavenumber domain (Wilczek and Narita, 2012). The effect of the sweeping velocity appears in the coefficient of the frequency spectrum.…”
Section: Discussionmentioning
confidence: 78%
“…The existence of Doppler broadening is confirmed both theoretically for a random sweeping model (Wilczek and Narita, 2012) and observationally in interplanetary space (Narita, 2014). Starting with the hydrodynamic treatment for Taylor's hypothesis, we develop a magnetohydrodynamic approach to Taylor's hypothesis with an application to the solar wind measurements of Doppler shift and broadening.…”
Section: Introductionmentioning
confidence: 99%
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“…Various models have been proposed to explain or reproduce the anisotropic energy spectra in the wavevector domain: the density fluctuation model (Higdon, 1984), the critical balance model by regulating the Alfvén wave interaction time with the eddy turnover time Sridhar, 1995, 1997;Forman et al, 2011), generalization of critical balance by adding damping (von Papen and Saur, 2015); two-component model consisting of slab geometry and quasi-two-dimensional turbulence (Matthaeus et al, 1990;Bieber et al, 1996), the three-component model as an extension of the two-component model by adding the compressible fluctuation component (Matthaeus and Ghosh, 1999), the cross-helicity model showing asymmetry in the energy spectrum between the parallel and the anti-parallel directions to the mean magnetic field (Chandran, 2008), and the elliptic anisotropy model parameterized by the shape coefficients (Carbone et al, 1995).…”
Section: Introductionmentioning
confidence: 99%