MMS Observations of a Compressed Current Sheet: Importance of the Ambipolar Electric Field

Ami M. DuBois, Chris Crabtree, Gurudas Ganguli, David M. Malaspina, and William E. Amatucci
Phys. Rev. Lett. 129, 105101 – Published 2 September 2022
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Abstract

Spacecraft data reveal a nonuniform ambipolar electric field transverse to the magnetic field in a thin current sheet in Earth’s magnetotail that leads to intense E×B velocity shear and nongyrotropic particle distributions. The E×B drift far exceeds the diamagnetic drift and thus drives observed lower hybrid waves. The shear-driven waves are localized to the magnetic field reversal region and are therefore ideally suited for the anomalous dissipation necessary for reconnection. It also reveals substructures embedded in the current density, indicating a compressed current sheet.

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  • Received 13 December 2021
  • Revised 15 July 2022
  • Accepted 12 August 2022
  • Corrected 6 September 2022

DOI:https://doi.org/10.1103/PhysRevLett.129.105101

Published by the American Physical Society

Physics Subject Headings (PhySH)

Plasma PhysicsParticles & Fields

Corrections

6 September 2022

Correction: The quantity L^ in the seventh paragraph (in “The total electron flow…”) was mistakenly set as EN during the production cycle and has been fixed.

Authors & Affiliations

Ami M. DuBois1, Chris Crabtree1, Gurudas Ganguli1, David M. Malaspina2,3, and William E. Amatucci1

  • 1U.S. Naval Research Laboratory, Plasma Physics Division, Washington, D.C. 20375-5346, USA
  • 2Astrophysical and Planetary Sciences Department, University of Colorado, Boulder, Colorado 80303-7814, USA
  • 3Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado 80303-7814, USA

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Issue

Vol. 129, Iss. 10 — 2 September 2022

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