2021
DOI: 10.1051/0004-6361/202140945
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Whistler waves observed by Solar Orbiter/RPW between 0.5 AU and 1 AU

Abstract: Context. Solar wind evolution differs from a simple radial expansion, while wave-particle interactions are assumed to be the major cause for the observed dynamics of the electron distribution function. In particular, whistler waves are thought to inhibit the electron heat flux and ensure the diffusion of the field-aligned energetic electrons (Strahl electrons) to replenish the halo population. Aims. The goal of our study is to detect and characterize the electromagnetic waves that have the capacity to modify t… Show more

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Cited by 27 publications
(28 citation statements)
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References 31 publications
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“…This finding is consistent with the observed lack of fast-magnetosonic/whistler waves in Parker Solar Probe data at heliocentric distances 0.13 au (Cattell et al, 2022). Moreover, the majority of the fast-magnetosonic/whistler waves observed farther away from the Sun have a quasi-parallel direction of propagation with respect to the magnetic field (Kretzschmar et al, 2021). Therefore, other mechanisms than the self-induced scattering of strahl electrons by the oblique fast-magnetosonic/whistler instability may thus be needed to explain the observed scattering of strahl electrons into the halo population (e.g., the interaction with pre-existing fastmagnetosonic/whistler waves; Vocks et al, 2005;Vocks and Mann, 2009;Pierrard et al, 2011;Jagarlamudi et al, 2021;Cattell and Vo, 2021;.…”
Section: Electron-driven Instabilitiessupporting
confidence: 89%
“…This finding is consistent with the observed lack of fast-magnetosonic/whistler waves in Parker Solar Probe data at heliocentric distances 0.13 au (Cattell et al, 2022). Moreover, the majority of the fast-magnetosonic/whistler waves observed farther away from the Sun have a quasi-parallel direction of propagation with respect to the magnetic field (Kretzschmar et al, 2021). Therefore, other mechanisms than the self-induced scattering of strahl electrons by the oblique fast-magnetosonic/whistler instability may thus be needed to explain the observed scattering of strahl electrons into the halo population (e.g., the interaction with pre-existing fastmagnetosonic/whistler waves; Vocks et al, 2005;Vocks and Mann, 2009;Pierrard et al, 2011;Jagarlamudi et al, 2021;Cattell and Vo, 2021;.…”
Section: Electron-driven Instabilitiessupporting
confidence: 89%
“…This finding is consistent with the observed lack of fastmagnetosonic/whistler waves in Parker Solar Probe data at heliocentric distances ≲ 0.13 au (Cattell et al, 2022). Moreover, the majority of the fast-magnetosonic/whistler waves observed farther away from the Sun have a quasiparallel direction of propagation with respect to the magnetic field (Kretzschmar et al, 2021). Therefore, other mechanisms than the self-induced scattering of strahl electrons by the oblique fast-magnetosonic/whistler instability may thus be needed to explain the observed scattering of strahl electrons into the halo population (e.g., the interaction with pre-existing fast-magnetosonic/whistler waves; Vocks et al, 2005;Vocks and Mann, 2009;Pierrard et al, 2011;Jagarlamudi et al, 2021;Cattell and Vo, 2021;.…”
Section: Oblique Fast-magnetosonic/whistler Instabilitysupporting
confidence: 88%
“…where V 23 and V 12 are the potential differences between probes 2 and 3 and 1 and 2, respectively, and L y = 6.99 m and L z = 6.97 m are the effective lengths in the y-and z-directions used in this paper. These effective lengths are based on the geometric lengths of the antennas and are in good agreement with estimates of the effective lengths based on deHoffman-Teller analysis using the DC electric and magnetic fields and comparing with the solar wind velocity (Steinvall et al 2021), along with a comparison of the electric and magnetic fields associated with whistler waves (Kretzschmar et al 2021). We apply this same calibration to both LFR and TDS potential data.…”
Section: Instruments and Datasupporting
confidence: 70%