REVIEW 2 cited by
Ion-Driven Instabilities in the Inner Heliosphere I: Statistical Trends
Not yet reviewed by Pith; the record is open.
This paper has not been read by Pith yet. Machine review is queued; the pith claim, tier, and objections will appear here once it completes.
SPECIMEN: schema-true, not a live event
T0 review · schema-true
One-sentence machine reading of the paper's core claim.
pith:XXXXXXXX · record.json · timestamp
abstract
Instabilities described by linear theory characterize an important form of wave-particle interaction in the solar wind. We diagnose unstable behavior of solar wind plasma between 0.3 and 1 au via the Nyquist criterion, applying it to fits of $\sim1.5$M proton and $\alpha$ particle Velocity Distribution Functions (VDFs) observed by \emph{Helios I} and \emph{II}. The variation of the fraction of unstable intervals with radial distance from the Sun is linear, signaling a gradual decline in the activity of unstable modes. When calculated as functions of the solar wind velocity and Coulomb number, we obtain more extreme, exponential trends in the regions where collisions appear to have a notable influence on the VDF. Instability growth rates demonstrate similar behavior, and significantly decrease with Coulomb number. We find that, for a non-negligible fraction of observations, the proton beam or secondary component might not be detected due to instrument resolution limitations, and demonstrate that the impact of this issue does not affect the main conclusions of this work.
Forward citations
Cited by 2 Pith papers
-
Impact of Two-Population $\alpha$-particle Distributions on Plasma Stability
Solar wind stability predictions match observed ion-scale wave signatures only when alpha particles are modeled as two populations (core and beam) rather than one.
-
On the transition from Slow to Fast Wind as Observed in Composition Observations
Heavy ion abundances suggest the slow-to-fast solar wind transition occurs at about 327 km/s, about 63 km/s slower than the helium-based transition, with a fast-wind abundance gradient ordered by element mass or charge state.
Discussion (0). Continue with ORCID to comment.