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Electron Inflow Velocities and Reconnection Rates at Earth's Magnetopause and Magnetosheath

  • J. L. Burch
  • , J. M. Webster
  • , M. Hesse
  • , K. J. Genestreti
  • , R. E. Denton
  • , T. D. Phan
  • , H. Hasegawa
  • , P. A. Cassak
  • , R. B. Torbert
  • , B. L. Giles
  • , D. J. Gershman
  • , R. E. Ergun
  • , C. T. Russell
  • , R. J. Strangeway
  • , O. Le Contel
  • , K. R. Pritchard
  • , A. T. Marshall
  • , K. J. Hwang
  • , K. Dokgo
  • , S. A. Fuselier
  • L. J. Chen, S. Wang, M. Swisdak, J. F. Drake, M. R. Argall, K. J. Trattner, M. Yamada, G. Paschmann
  • Southwest Research Institute
  • Rice University
  • University of Bergen
  • Dartmouth College
  • University of California, Space Sciences Laboratory
  • ISAS/JAXA
  • West Virginia University
  • University of New Hampshire
  • NASA Goddard Space Flight Center
  • University of Colorado Boulder
  • Institute of Geophysics and Planetary Physics, University of California
  • University of Texas
  • University of Maryland
  • University of Maryland
  • Princeton Plasma Physics Laboratory
  • Max Planck Institut für Extraterrestrische Physik

Résultats de recherche: Contribution à un journalArticleRevue par des pairs

39 Citations (Scopus)

Résumé

Electron inflow and outflow velocities during magnetic reconnection at and near the dayside magnetopause are measured using satellites from NASA's Magnetospheric Multiscale (MMS) mission. A case study is examined in detail, and three other events with similar behavior are shown, with one of them being a recently published electron-only reconnection event in the magnetosheath. The measured inflow speeds of 200–400 km/s imply dimensionless reconnection rates of 0.05–0.25 when normalized to the relevant electron Alfvén speed, which are within the range of expectations. The outflow speeds are about 1.5–3 times the inflow speeds, which is consistent with theoretical predictions of the aspect ratio of the inner electron diffusion region. A reconnection rate of 0.04 ± 25% was obtained for the case study event using the reconnection electric field as compared to the 0.12 ± 20% rate determined from the inflow velocity.

langue originaleAnglais
Numéro d'articlee2020GL089082
journalGeophysical Research Letters
Volume47
Numéro de publication17
Les DOIs
étatPublié - 16 sept. 2020

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