Whistler instability driven by the sunward electron deficit in the solar wind
Laura Ber\v{c}i\v{c}, Daniel Verscharen, Christopher J. Owen, Lucas, Colomban, Matthieu Kretzschmar, Thomas Chust, Milan Maksimovi\'c, Dhiren, Kataria, Etienne Behar, Matthieu Berthomier, Roberto Bruno, Vito Fortunato,, Christopher W. Kelly, Yuri. V. Khotyaintsev

TL;DR
This study investigates how a sunward electron deficit in the solar wind triggers whistler wave instabilities, using Solar Orbiter data to identify quasi-parallel whistler waves associated with this deficit.
Contribution
It demonstrates the direct link between sunward electron deficits and the generation of whistler waves in the solar wind through combined observational analysis.
Findings
Detected quasi-parallel whistler waves propagating away from the Sun.
Confirmed the sunward electron deficit correlates with whistler wave activity.
Validated the cyclotron-resonance condition for electrons in the observed waves.
Abstract
Solar wind electrons play an important role in the energy balance of the solar wind acceleration by carrying energy into interplanetary space in the form of electron heat flux. The heat flux is stored in the complex electron velocity distribution functions (VDFs) shaped by expansion, Coulomb collisions, and field-particle interactions. We investigate how the suprathermal electron deficit in the anti-strahl direction, which was recently discovered in the near-Sun solar wind, drives a kinetic instability and creates whistler waves with wave vectors that are quasi-parallel to the direction of the background magnetic field. We combine high-cadence measurements of electron pitch-angle distribution functions and electromagnetic waves provided by Solar Orbiter during its first orbit. Our case study is based on a burst-mode data interval from the Electrostatic Analyser System (SWA-EAS) at a…
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