Interaction between inclined current sheets and the heliospheric termination shock

15Citations
Citations of this article
10Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

Using two-dimensional hybrid simulations we study the interaction between the Heliospheric Current Sheet (HCS) and the solar wind termination shock (TS). Hot flow anomalies (HFA) are regions of hot, deflected and disturbed plasma flow which may form at the intersection of a shock and current sheet. We study the role played by the inclination, θ Cn, of the current sheet relative to the shock normal. As previously found, low values of θ Cn are associated with HFA formation. We find that as θ Cn increases the HFA is modified, until at θ Cn = 60 it disappears completely. Thus, HFAs are unlikely to be formed near the TS since the HCS is highly inclined relative to the radial direction (θ Cn 60). We also find that some suprathermal particles, particularly interstellar pickup ions, are trapped near the intersection point of the shock and current sheet where they gain considerable energy, and subsequently drift along the current sheet upstream of the shock. This process is more effective for larger values of θ Cn. Thus, we expect that upstream of the TS there are likely to be high-energy particles (energized pickup ions) associated with crossings of the HCS, but only of the particular magnetic reversal polarity associated with HFAs. This may be relevant to recently reported Voyager observations. © 2010 by the American Geophysical Union.

Cite

CITATION STYLE

APA

Giacalone, J., & Burgess, D. (2010). Interaction between inclined current sheets and the heliospheric termination shock. Geophysical Research Letters, 37(19). https://doi.org/10.1029/2010GL044656

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free