paper

The Radial Distribution of Ion-scale Waves in the Inner Heliosphere

arXiv:2305.08424 · doi:10.3847/1538-4357/acd53b

Abstract

Determining the mechanism responsible for the plasma heating and particle acceleration is a fundamental problem in the study of the heliosphere. Due to efficient wave-particle interactions of ion-scale waves with charged particles, these waves are widely believed to be a major contributor to ion energization, and their contribution considerably depends on the wave occurrence rate. By analyzing the radial distribution of quasi-monochromatic ion-scale waves observed by the Parker Solar Probe, this work shows that the wave occurrence rate is significantly enhanced in the near-Sun solar wind, specifically 21%29% below 0.3 au, in comparison to 6%14% beyond 0.3 au. The radial decrease of the wave occurrence rate is not only induced by the sampling effect of a single spacecraft detection, but also by the physics relating to the wave excitation, such as the enhanced ion beam instability in the near-Sun solar wind. This work also shows that the wave normal angle , the absolute value of ellipticity , the wave frequency normalized by the proton cyclotron frequency , and the wave amplitude normalized by the local background magnetic field slightly vary with the radial distance. The median values of , , , and are about , , , and , respectively. Furthermore, this study proposes that the wave mode nature of the observed left-handed and right-handed polarized waves corresponds to the Alfvén ion cyclotron mode wave and the fast-magnetosonic whistler mode wave, respectively.

Accepted for publication by The Astrophysical Journal (ApJ)

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