Whistler waves generated inside magnetic dips in the young solar wind: Observations of the search-coil magnetometer on board Parker Solar Probe

¹ LPC2E, CNRS/University of Orléans/CNES, 3A avenue de la Recherche Scientifique, Orléans, France
e-mail: clara.froment@cnrs-orleans.fr
² Space Sciences Laboratory, University of California, Berkeley, CA 94720-7450, USA
³ International Space Science Institute, ISSI, Bern, Switzerland
⁴ Department of Physics and Astronomy, Queen Mary University of London, London, UK
⁵ Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO 80303, USA
⁶ Astrophysical and Planetary Sciences Department, University of Colorado, Boulder, CO 80303, USA
⁷ Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA
⁸ Physics Department, University of California, Berkeley, CA, USA

Received: 5 October 2022
Accepted: 2 February 2023

Abstract

Context. Whistler waves are electromagnetic waves produced by electron-driven instabilities, which in turn can reshape the electron distributions via wave–particle interactions. In the solar wind they are one of the main candidates for explaining the scattering of the strahl electron population into the halo at increasing radial distances from the Sun and for subsequently regulating the solar wind heat flux. However, it is unclear what type of instability dominates to drive whistler waves in the solar wind.

Aims. Our goal is to study whistler wave parameters in the young solar wind sampled by Parker Solar Probe (PSP). The wave normal angle (WNA) in particular is a key parameter to discriminate between the generation mechanisms of these waves.

Methods. We analyzed the cross-spectral matrices of magnetic field fluctuations measured by the search-coil magnetometer (SCM) and processed by the Digital Fields Board (DFB) from the FIELDS suite during PSP’s first perihelion.

Results. Among the 2701 wave packets detected in the cross-spectra, namely individual bins in time and frequency, most were quasi-parallel to the background magnetic field; however, a significant part (3%) of the observed waves had oblique (> 45°) WNA. The validation analysis conducted with the time series waveforms reveal that this percentage is a lower limit. Moreover, we find that about 64% of the whistler waves detected in the spectra are associated with at least one magnetic dip.

Conclusions. We conclude that magnetic dips provide favorable conditions for the generation of whistler waves. We hypothesize that the whistlers detected in magnetic dips are locally generated by the thermal anisotropy as quasi-parallel and can gain obliqueness during their propagation. We finally discuss the implications of our results for the scattering of the strahl in the solar wind.