Nature of stochastic ion heating in the solar wind: testing the dependence on plasma beta and turbulence amplitude
Daniel Vech, Kristopher G. Klein, Justin C. Kasper

TL;DR
This study tests stochastic ion heating in the solar wind, revealing its dependence on plasma beta and turbulence amplitude, and finds it likely operates most of the time at 1 AU.
Contribution
First statistical test of stochastic ion heating dependence on plasma beta and turbulence amplitude in solar wind data.
Findings
Proton temperature enhancement occurs above a critical turbulence amplitude.
Temperature increases depend on plasma beta, with different behaviors for low and high beta.
Stochastic heating likely operates in most solar wind conditions at 1 AU.
Abstract
The solar wind undergoes significant heating as it propagates away from the Sun; the exact mechanisms responsible for this heating are not yet fully understood. We present for the first time a statistical test for one of the proposed mechanisms, stochastic ion heating. We use the amplitude of magnetic field fluctuations near the proton gyroscale as a proxy for the ratio of gyroscale velocity fluctuations to perpendicular (with respect to the magnetic field) proton thermal speed, defined as . Enhanced proton temperatures are observed when is larger than a critical value (). This enhancement strongly depends on the proton plasma beta (); when only the perpendicular proton temperature increases, while for increased parallel and perpendicular proton temperatures are both observed.…
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