New Insight into Short-Wavelength Solar Wind Fluctuations from Vlasov Theory

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Citation of Original Publication

Sahraoui, F., G. Belmont, and M. L. Goldstein. “New Insight into Short-Wavelength Solar Wind Fluctuations from Vlasov Theory.” The Astrophysical Journal 748, no. 2 (March 2012): 100. https://doi.org/10.1088/0004-637X/748/2/100.

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This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
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Abstract

The nature of solar wind (SW) turbulence below the proton gyroscale is a topic that is being investigated extensively nowadays, both theoretically and observationally. Although recent observations gave evidence of the dominance of kinetic Alfvén waves (KAWs) at sub-ion scales with ω < ωcᵢ, other studies suggest that the KAW mode cannot carry the turbulence cascade down to electron scales and that the whistler mode (i.e., ω > ωcᵢ) is more relevant. Here, we study key properties of the short-wavelength plasma modes under limited, but realistic, SW conditions, typically βᵢ ≳ βₑ ∼ 1 and for high oblique angles of propagation 80° ⩽ ΘkB < 90° as observed from the Cluster spacecraft data. The linear properties of the plasma modes under these conditions are poorly known, which contrasts with the well-documented cold plasma limit and/or moderate oblique angles of propagation (ΘkB < 80°). Based on linear solutions of the Vlasov kinetic theory, we discuss the relevance of each plasma mode (fast, Bernstein, KAW, whistler) in carrying the energy cascade down to electron scales. We show, in particular, that the shear Alfvén mode (known in the magnetohydrodynamic limit) extends at scales kρᵢ ≳ 1 to frequencies either larger or smaller than ωcᵢ, depending on the anisotropy k∥/k⊥. This extension into small scales is more readily called whistler (ω > ωcᵢ) or KAW (ω < ωcᵢ), although the mode is essentially the same. This contrasts with the well-accepted idea that the whistler branch always develops as a continuation at high frequencies of the fast magnetosonic mode. We show, furthermore, that the whistler branch is more damped than the KAW one, which makes the latter the more relevant candidate to carry the energy cascade down to electron scales. We discuss how these new findings may facilitate resolution of the controversy concerning the nature of the small-scale turbulence, and we discuss the implications for present and future spacecraft wave measurements in the SW.