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Cyclotron breaking: a mechanism for parallel ion cyclotron waves to heat the fast solar wind

Published online by Cambridge University Press:  08 July 2026

Evan L. Yerger*
Affiliation:
Space Science Center, University of New Hampshire , Durham, NH 03824, USA
Benjamin D.G. Chandran
Affiliation:
Space Science Center, University of New Hampshire , Durham, NH 03824, USA Department of Physics, University of New Hampshire, Durham, NH 03824, USA
Vincent David
Affiliation:
Space Science Center, University of New Hampshire , Durham, NH 03824, USA Department of Physics and Astronomy, Dartmouth College, Hanover, NH 03755, USA
Trevor A. Bowen
Affiliation:
Space Sciences Laboratory, University of California, Berkeley, CA 94720, USA
Stuart D. Bale
Affiliation:
Space Sciences Laboratory, University of California, Berkeley, CA 94720, USA Physics Department, University of California, Berkeley, CA 94720, USA
*
Corresponding author: Evan L. Yerger, evan.yerger@unh.edu

Abstract

The Parker Solar Probe mission has observed near-continuous power in parallel ion cyclotron waves (PICWs) in the young, fast solar wind. These waves are unlikely to be directly produced by the turbulent cascade and are likely born of a local instability; yet, they are observed to both cool – and heat – the plasma. We propose that these observations can be self-consistently explained as the natural consequence of PICWs propagating in the inhomogeneous solar wind after they have been driven unstable. In this work, we argue that strong proton heating by a turbulent cascade of oblique ICWs will result in PICWs being driven unstable in a process known as quasi-linear focusing. Because the power in the turbulent cascade is concentrated at scales above the turbulent transition region, PICWs will be driven unstable within a range of wavenumbers parallel to the background magnetic field, $k_\parallel$, that is bounded from above by $k_{\parallel {\mathrm{P}}}^*$, corresponding to the start of the transition region. As unstable PICWs propagate away from the Sun to regions of lower proton density, their $k_\parallel$, multiplied by the proton inertial length $d_{\mathrm{p}}$, increases. Eventually, $k_\parallel d_{\mathrm{p}}$ of the PICWs becomes larger than $k_{\parallel {\mathrm{P}}}^*d_{\mathrm{p}}$ and the waves damp, heating the solar wind. We call this effect ‘cyclotron breaking’, in analogy with ocean waves breaking on the shore. We then discuss the testable predictions of the theory, including a distinct heating signature in which PICWs cool fast protons and heat slow protons at any given heliocentric distance $r$. Finally, we conjecture that cyclotron breaking can lead to net heating by PICWs if the power emitted as PICWs decreases sufficiently rapidly with $r$ that local emission of PICWs is overwhelmed by the local damping of PICWs generated closer to the Sun.

Information

Type
Letter
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1. The frequency of an oblique ICW, ωk∥r,O$\omega _{k_\parallel {\mathrm{r}},{\rm O}}$, here with (a very exaggerated value of) k⊥dp=10$k_\perp d_{\mathrm{p}}=10$, is always larger than ωk∥r,P$\omega _{k_\parallel {\mathrm{r}},{\rm P}}$ for a given k∥$k_\parallel$. As a result, k∥P>k∥O$k_{\parallel {\mathrm{P}}}\gt k_{\parallel {\mathrm{O}}}$, as shown by the intersection of ωkr,O$\omega _{k{\mathrm{r}},{\rm O}}$ and ωk∥r,P$\omega _{k_\parallel {\mathrm{r}},{\rm P}}$ with Ωp+k∥v∥$\varOmega _{\mathrm{p}}+k_\parallel v_\parallel$ in (a). One can then show that (ωk∥r,O/k∥)|k∥O−(ωk∥r,P/k∥)|k∥P>0$(\omega _{k_\parallel {\mathrm{r}},{\rm O}}/k_\parallel )|_{k_{\parallel \mathrm{O}}}-(\omega _{k_\parallel {\mathrm{r}},{\rm P}}/k_\parallel )|_{k_{\parallel {\mathrm{P}}}}\gt 0$ (see text), a necessary condition for quasi-linear focusing. For this condition to be sufficient, the proton velocity distribution must be nearly constant along oblique ICW contours. In (b) (after figure 4 in Chandran et al.(2010b)), we show the proton velocity distribution function (darker purple denotes contours of higher particle density) only for v∥$v_\parallel \lt v_\parallel ^*$, where v∥∗$v_\parallel ^*$ is the resonant parallel velocity associated with the start of the turbulent transition region (see § 3.2). Physically, PICWs provide alternative quasi-linear contours (black semicircles) along which protons can diffuse. Because (ωk∥r,O/k∥)|k∥O−(ωk∥r,P/k∥)|k∥P>0$(\omega _{k_\parallel {\mathrm{r}},{\rm O}}/k_\parallel )|_{k_{\parallel \mathrm{O}}}-(\omega _{k_\parallel {\mathrm{r}},{\rm P}}/k_\parallel )|_{k_{\parallel {\mathrm{P}}}}\gt 0$ (the difference in (b) is exaggerated for clarity), protons will on average diffuse towards regions of velocity space with lower proton density, i.e. in the direction given by the black arrow. These regions of low proton density also have lower energy (contours of larger constant energy are given by darker orange semicircles); the energy lost by protons is given to the PICWs, causing their amplitude to grow (Chandran et al.2010b). Purple, black and orange dashed lines, corresponding to the centre of the semicircular quasi-linear contours for oblique ICWs, PICWs and contour of constant energy, respectively, are included to aid the eye.

Figure 1

Figure 2. A reduced magnetic fluctuation spectrum EδB(k⊥)$\mathcal{E}_{\delta B}(k_\perp )$, typical of the solar wind. The transition range (TR), characterised by a steep ∼k⊥−4${\sim }k_\perp ^{-4}$ spectral slope, is sandwiched between the inertial range (IR) and kinetic-Alfvén-wave range (KAW). We denote the perpendicular wavenumber at the boundary between the IR and TR as k⊥∗$k_\perp ^*$.

Figure 2

Figure 3. A diagrammatic description of quasi-linear focusing in the presence of the turbulent transition range. Our model turbulent spectrum for δB$\delta B$ is shown in (a), with darker green denoting larger values. The perpendicular and parallel start of the transition range, k⊥∗$k_\perp ^*$ and k∥∗$k_\parallel ^*$, and the critical balance anisotropy relationship k∥,CB(k⊥)$k_{\parallel ,\mathrm{CB}}(k_\perp )$ are given by the vertical, horizontal and slanted dashed black lines, respectively. Heating by the cascade (red circle in a) pushes the proton velocity distribution fp$f_{\mathrm{p}}$, shown in (b), constant along oblique ICW quasi-linear contours for v∥$v_\parallel \lt v_\parallel ^*$, where v∥∗$v_\parallel ^*$ is the resonant parallel velocity for an oblique ICW with k∥=k∥∗$k_\parallel =k_\parallel ^*$ and k⊥=k⊥∗$k_\perp =k_\perp ^*$. Here, fp$f_{\mathrm{p}}$ is unstable to PICWs because oblique ICW quasi-linear contours are steeper than PICW contours (given by black lines in b). The PICWs will therefore be emitted, cooling fp$f_{\mathrm{p}}$, in the wavenumber region given by the blue circle in (a). For v∥>v∥∗$v_\parallel \gt v_\parallel ^*$, fp$f_{\mathrm{p}}$ is much more isotropic because heating by oblique ICWs is much weaker there. Consequently, the contours of fp$f_{\mathrm{p}}$ are shallower than those of the PICWs, and the PICWs are damped. A given unstable PICW, resonating with protons with v∥$v_\parallel$ given by the vertical blue line in (b), will necessarily have k∥$k_\parallel \lt k_{\parallel {\mathrm{P}}}^*\simeq k_\parallel ^*$. (c) The PICW resonance diagram shows ωk∥r,P$\omega _{k_\parallel {\mathrm{r,P}}}$ (black curved line) and the right-hand side of (3.2) (straight lines) – the intersection of which is the solution to the resonance condition. Wave–particle interactions with faster protons constitute steeper lines and therefore smaller resonant k∥$k_\parallel$. We approximate the extent of the excited spectrum of PICWs by the blue circle in (a).

Figure 3

Figure 4. Parallel ICWs driven unstable by quasi-linear focusing in the vicinity of the turbulent transition range cool the solar wind (see figure 3). The PICWs that are at one radius unstable will propagate away from the Sun. As they do, the wave frequency and parallel wave vector will evolve according to (3.4), i.e. along the (properly normalised) PICW dispersion relation towards larger values, as shown by the arrow in (c). The solution to the resonance condition changes appropriately, with PICWs resonating with slower and slower protons as they propagate – shown by the red line in (b). At some point in their anti-sunward trajectory, the PICWs will begin to resonate with the v∥>v∥∗$v_\parallel \gt v_\parallel ^*$ part of the proton velocity distribution (which has not been heated by the ICW cascade) and will be damped. The damped waves heat the solar wind, as emphasised by the red lines in (b, c). We also approximate the wavenumber spectrum of damped PICWs with a red circle at k∥≳k∥∗$k_\parallel \gtrsim k_\parallel ^*$ in (a).