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 velocity shear and nongyrotropic particle distributions. The 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.
- 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)
Corrections
6 September 2022
Correction: The quantity in the seventh paragraph (in “The total electron flow…”) was mistakenly set as during the production cycle and has been fixed.