On the transition from Slow to Fast Wind as Observed in Composition Observations

TL;DR

This study investigates the transition between slow and fast solar wind by analyzing heavy ion abundances, revealing nuanced differences in transition speeds and potential fractionation processes affecting heavy ions.

Contribution

It provides new insights into the speed-dependent transition between slow and fast solar wind using heavy ion data, challenging the traditional binary classification.

Findings

Heavy ion abundance transition speed is slower than helium-based transition.

Transition speed is independent of heavy ion mass and charge.

Heavy ions show potential mass or charge-state dependent fractionation.

Abstract

The solar wind is typically categorized as fast and slow based on the measured speed ($v_\mathrm{sw}$). The separation between these two regimes is often set between 400 and 600 km/s without a rigorous definition. Observations of the solar wind's kinetic signatures, chemical makeup, charge state properties, and Alfv\'enicity suggest that such a two-state model may be insufficiently nuanced to capture the relationship between the solar wind and its solar sources. We test this two-state fast/slow solar wind paradigm with heavy ion abundances (X/H) and characterize how the transition between fast and slow wind states impacts heavy ion in the solar wind. We show that (1) the speed at which heavy ion abundances indicate a change between fast and slow solar wind as a function of speed is slower than the speed indicated by the helium abundance; (2) this speed is independent of heavy ion mass and charge state; (3) the abundance at which heavy ions indicate the transition between fast and slow wind is consistent with prior observations of fast wind abundances; (4) and there may be a mass or charge-state dependent fractionation process present in fast wind heavy ion abundances. We infer that (1) identifying slow solar wind as having a speed $v_\mathrm{sw} \lesssim$ 400 km/s may mix solar wind from polar and equatorial sources; (2) He may be impacted by the acceleration necessary for the solar wind to reach the asymptotic fast, non-transient values observed at 1 AU; and (3) heavy ions are fractionated in the fast wind by a yet-to-be-determined mechanism.