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Title: Electron Diffusion Regions in Magnetotail Reconnection Under Varying Guide Fields

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2019GL082393· OSTI ID:1560205
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [5]; ORCiD logo [6]; ORCiD logo [7]; ORCiD logo [8]; ORCiD logo [1]; ORCiD logo [9]; ORCiD logo [10]; ORCiD logo [11]; ORCiD logo [5]; ORCiD logo [12]; ORCiD logo [13]
  1. NASA, Goddard Space Flight Center Greenbelt MD USA
  2. NASA, Goddard Space Flight Center Greenbelt MD USA, Department of Astronomy University of Maryland College Park MD USA
  3. Department of Physics and Technology University of Bergen Bergen Norway
  4. Laboratory of Atmospheric and Space Sciences University of Colorado Boulder Boulder CO USA
  5. Department of Earth, Planetary, and Space Sciences University of California Los Angeles CA USA
  6. Southwest Research Institute San Antonio TX USA
  7. Southwest Research Institute San Antonio TX USA, Space Science Center University of New Hampshire Durham NH USA
  8. Space Science Center University of New Hampshire Durham NH USA
  9. Denali Scientific Healy AK USA
  10. Institut de Recherche en Astrophysique et Planétologie, Université de Toulouse (UPS), CNRS, CNES Toulouse France
  11. Laboratoire de Physique des Plasmas (UMR7648), CNRS/Ecole Polytechnique/Sorbonne Université/Univ. Paris‐Sud/Observatoire de Paris Paris France
  12. Swedish Institute of Space Physics Uppsala Sweden
  13. KTH Royal Institute of Technology Stockholm Sweden

Abstract Kinetic structures of electron diffusion regions (EDRs) under finite guide fields in magnetotail reconnection are reported. The EDRs with guide fields 0.14–0.5 (in unit of the reconnecting component) are detected by the Magnetospheric Multiscale spacecraft. The key new features include the following: (1) cold inflowing electrons accelerated along the guide field and demagnetized at the magnetic field minimum while remaining a coherent population with a low perpendicular temperature, (2) wave fluctuations generating strong perpendicular electron flows followed by alternating parallel flows inside the reconnecting current sheet under an intermediate guide field, and (3) gyrophase bunched electrons with high parallel speeds leaving the X‐line region. The normalized reconnection rates for the three EDRs range from 0.05 to 0.3. The measurements reveal that finite guide fields introduce new mechanisms to break the electron frozen‐in condition.

Research Organization:
Univ. of Maryland, College Park, MD (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
SC0016278
OSTI ID:
1560205
Alternate ID(s):
OSTI ID: 1560207; OSTI ID: 1844382
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Vol. 46 Journal Issue: 12; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 25 works
Citation information provided by
Web of Science

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