Candidates for downstream jets at interplanetary shocks

Author:

Hietala H123ORCID,Trotta D2ORCID,Fedeli A3,Wilson L B4,Vuorinen L3,Coburn J T56

Affiliation:

1. Department of Physics and Astronomy, Queen Mary University of London , Mile End Road, London E1 4NS , UK

2. The Blackett Laboratory, Department of Physics, Imperial College London , Prince Consort Road, London SW7 2AZ , UK

3. Department of Physics and Astronomy, University of Turku , Vesilinnantie 5, Fl-20500 Turku , Finland

4. NASA Goddard Space Flight Center , Greenbelt, MD 20771 , USA

5. Mullard Space Science Laboratory, University College London , Holmbury St. Mary, Dorking RH5 6NT , UK

6. Space Science Institute , 4765 Walnut St, Suite B, Boulder, CO 80301 , USA

Abstract

ABSTRACT Localized dynamic pressure enhancements arising from kinetic processes are frequently observed downstream of the Earth’s bow shock. These structures, called jets, modify their plasma surroundings and participate in particle energization. Here, we report the first observations of jet-like structures in a non-planetary shock environment: downstream of interplanetary shocks. We introduce an analysis approach suitable for such conditions and apply it to Wind spacecraft data. We present one event with a Mach number similar to the Earth’s bow shock as a benchmark, as well as two low Mach number, low beta shocks: a parameter range that is difficult to access at planets. The jet-like structures we find are tens of ion inertial lengths in size, and some are observed further away from the shock than in a limited magnetosheath. We find that their properties are similar to those of magnetosheath jets: in the frame of the shock these structures are fast, cold, and most have no strong magnetic field variations. All three interplanetary shocks feature foreshock activity, but no strongly compressive waves. We discuss the implications, these findings have for the proposed jet formation mechanisms.

Funder

Horizon 2020

Publisher

Oxford University Press (OUP)

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