Structure and fluctuations of a slow ICME sheath observed at 0.5 au by the Parker Solar Probe

TL;DR

This study analyzes the structure and turbulence of a slow ICME sheath at 0.5 au using Parker Solar Probe data, revealing complex internal fluctuations and a two-part sheath structure influenced by the heliospheric current sheet.

Contribution

It provides detailed turbulence analysis of a slow ICME sheath at 0.5 au, highlighting internal structure and fluctuation properties not solely due to shocks.

Findings

Sheath had higher fluctuation amplitudes and PVI than upstream wind.

Sheath fluctuations showed lower entropy and higher complexity.

Two-part sheath structure linked to HCS warp and wind interactions.

Abstract

Sheaths ahead of interplanetary coronal mass ejections (ICMEs) are turbulent heliospheric structures. Knowledge of their structure and fluctuations is important for understanding their geoeffectiveness, their role in accelerating particles, and the interaction of ICMEs with the solar wind. We studied observations from the Parker Solar Probe of a sheath observed at 0.5 au in March 2019, ahead of a slow streamer blowout CME. To examine the MHD-scale turbulent properties, we calculated fluctuation amplitudes, magnetic compressibility, partial variance of increments (PVI), cross helicity ($\sigma_c$), residual energy ($\sigma_r$), and the Jensen-Shannon permutation entropy and complexity. The sheath consisted of slow and fast flows separated by a 15-min change in magnetic sector that coincided with current sheet crossings and a velocity shear zone. Fluctuation amplitudes and PVI were greater through the sheath than upstream. Fluctuations had mostly negative $\sigma_r$ and positive $\sigma_c$ in the sheath, the latter indicating an anti-sunward sense of propagation. The velocity shear region marked an increase in temperature and specific entropy, and the faster flow behind had local patches of positive $\sigma_r$ as well as higher fluctuation amplitudes and PVI. Fluctuations in the preceding wind and sheath were stochastic, with the sheath fluctuations showing lower entropy and higher complexity than upstream. The two-part sheath structure likely resulted from a warp in the heliospheric current sheet (HCS) being swept up and compressed. The ejecta accelerated and heated the wind at the sheath rear, which then interacted with the slower wind ahead of the HCS warp. This caused differences in fluctuation properties across the sheath. Sheaths of slow ICMEs can thus have complex structure where fluctuation properties are not just downstream shock properties, but are generated within the sheath.