2004
DOI: 10.1103/revmodphys.76.1015
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Colloquium: Magnetohydrodynamic turbulence and time scales in astrophysical and space plasmas

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Cited by 234 publications
(251 citation statements)
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References 96 publications
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“…Simulation results [3,28,36,55,56] and phenomenologies [29,35,57,58] support the notion that small scales are more anisotropic, and achieve their quasitwo-dimensional-type states more rapidly than larger scales.…”
Section: (A) Review Of Observationsmentioning
confidence: 48%
“…Simulation results [3,28,36,55,56] and phenomenologies [29,35,57,58] support the notion that small scales are more anisotropic, and achieve their quasitwo-dimensional-type states more rapidly than larger scales.…”
Section: (A) Review Of Observationsmentioning
confidence: 48%
“…This represents that the large-angle current sheets may originate from a different mechanism from the small-angle population. The first approximate log-normal distribution is similar to the result of Miao, Peng, and Li (2011); this result shows that there are perhaps small-angle current sheets that developed in the solar-wind MHD turbulence, as shown by Zhou, Matthaeus, and Dmitruk (2004) and Chang, Tam, and Wu (2004). Therefore, these current sheets may represent the intrinsic intermittency of the solar-wind MHD turbulence.…”
supporting
confidence: 57%
“…For example, numerical MHD simulations by Zhou, Matthaeus, and Dmitruk (2004) and Chang, Tam, and Wu (2004) showed that current sheets can emerge from the dynamical evolution of the nonlinear interactions of the solar-wind MHD turbulence. All of these studies suggested that the current sheet is an intrinsic property of the solar-wind MHD turbulence.…”
Section: Introductionmentioning
confidence: 99%
“…A naive modeling is W + 2 Z − /l, where l is the characteristic length scale of the wave-like component. In fact, a multiplicative factor should be included to account for the shortening of the triple correlation time scale (see equation (A4)) associated with the wave-like propagation effects for this nonlinear term [Kraichnan, 1965;Grappin et al, 1982Grappin et al, , 1983Matthaeus and Zhou, 1989;Zhou et al, 2004]. Generically, these factors are G = (1 + t nl /t A ) −1 < 1, so that for this example term our modeling yields G z zw W + 2 Z − /l.…”
Section: Incompressible Two-component Turbulence Modelmentioning
confidence: 99%