Narrowband oblique whistler-mode waves: Comparing properties observed by Parker Solar Probe at <0.2 AU and STEREO at 1 AU
C. Cattell, B. Short, A. Breneman, J. Halekas, P. Whittesley, J., Kasper, Mike Stevens, Tony Case, M. Moncuquet, S. Bale, J. Bonnell, T. Dudok, de Wit, K. Goetz, P. Harvey, R. MacDowall, D. Malaspina, M. Pulupa, K., Goodrich

TL;DR
This study compares narrowband oblique whistler-mode waves observed by Parker Solar Probe inside 0.2 AU with those at 1 AU, revealing their properties, variability, and potential role in regulating electron heat flux in the solar wind.
Contribution
It provides the first detailed comparison of whistler-mode wave properties inside 0.2 AU with those at 1 AU, highlighting differences in intermittency and wave characteristics.
Findings
Waves are more intermittent closer to the Sun.
Whistler waves are associated with beta > 1 and regulate electron heat flux.
Wave angles are often highly oblique, near the resonance cone.
Abstract
AIM: Large amplitude narrowband obliquely propagating whistler-mode waves at frequencies of ~0.2 fce (electron cyclotron frequency) are commonly observed at 1 AU, and are most consistent with the whistler heat flux fan instability. We want to determine whether similar whistler-mode waves occur inside 0.2 AU, and how their properties compare to those at 1 AU. METHODS: We utilize the waveform capture data from the Parker Solar Probe Fields instrument to develop a data base of narrowband whistler waves. The SWEAP instrument, in conjunction with the quasi-thermal noise measurement form Fields, provides the electron heat flux, beta, and other electron parameters. RESULTS: Parker Solar Probe observations inside ~0.3 AU show that the waves are more intermittent than at 1 AU, and are often interspersed with electrostatic whistler/Bernstein waves at higher frequencies. This is likely due to…
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