Electron-ion heating partition in imbalanced solar-wind turbulence
Jonathan Squire, Romain Meyrand, Matthew W. Kunz

TL;DR
This paper investigates how the imbalance in Alfvénic turbulence influences ion and electron heating in the solar wind, revealing that low imbalance shifts energy from ions to electrons and aligns with observed solar wind features.
Contribution
It introduces a hybrid-kinetic simulation demonstrating the impact of turbulence imbalance on heating mechanisms and the dissipation of the helicity barrier in solar wind plasma.
Findings
Imbalance reduction leads to increased electron and parallel ion heating.
Dissolution of the helicity barrier correlates with observed spectral features.
Predictions align with diverse solar wind observations.
Abstract
A likely candidate mechanism to heat the solar corona and solar wind is low-frequency "Alfv\'enic" turbulence sourced by magnetic fluctuations near the solar surface. Depending on its properties, such turbulence can heat different species via different mechanisms, and the comparison of theoretical predictions to observed temperatures, wind speeds, anisotropies, and their variation with heliocentric radius provides a sensitive test of this physics. Here we explore the importance of normalized cross helicity, or imbalance, for controlling solar-wind heating, since it is a key parameter of magnetized turbulence and varies systematically with wind speed and radius. Based on a hybrid-kinetic simulation in which the forcing's imbalance decreases with time -- a crude model for a plasma parcel entrained in the outflowing wind -- we demonstrate how significant changes to the turbulence and…
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Taxonomy
TopicsSolar and Space Plasma Dynamics · Ionosphere and magnetosphere dynamics · Geomagnetism and Paleomagnetism Studies
