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Title: On the formation and origin of substorm growth phase/onset auroral arcs inferred from conjugate space-ground observations

Journal Article · · Journal of Geophysical Research. Space Physics
DOI:https://doi.org/10.1002/2015JA021676· OSTI ID:1236775
 [1];  [2];  [2];  [2];  [2];  [3];  [4];  [5];  [6];  [7]
  1. The Johns Hopkins Univ. Applied Physics Lab., Laurel, MD (United States); Nagoya Univ., Nagoya (Japan)
  2. The Johns Hopkins Univ. Applied Physics Lab., Laurel, MD (United States)
  3. New Jersey Institute of Technology, Newark, NJ (United States)
  4. Nagoya Univ., Nagoya (Japan)
  5. Athabasca Univ., Athabasca, AB (Canada)
  6. Univ. of Iowa, Iowa City, IA (United States)
  7. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

In this study, magnetotail processes and structures related to substorm growth phase/onset auroral arcs remain poorly understood mostly due to the lack of adequate observations. In this study we make a comparison between ground-based optical measurements of the premidnight growth phase/onset arcs at subauroral latitudes and magnetically conjugate measurements made by the Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) at ~780 km in altitude and by the Van Allen Probe B (RBSP-B) spacecraft crossing L values of ~5.0–5.6 in the premidnight inner tail region. The conjugate observations offer a unique opportunity to examine the detailed features of the arc location relative to large-scale Birkeland currents and of the magnetospheric counterpart. Our main findings include (1) at the early stage of the growth phase the quiet auroral arc emerged ~4.3° equatorward of the boundary between the downward Region 2 (R2) and upward Region 1 (R1) currents; (2) shortly before the auroral breakup (poleward auroral expansion) the latitudinal separation between the arc and the R1/R2 demarcation narrowed to ~1.0°; (3) RBSP-B observed a magnetic field signature of a local upward field-aligned current (FAC) connecting the arc with the near-Earth tail when the spacecraft footprint was very close to the arc; and (4) the upward FAC signature was located on the tailward side of a local plasma pressure increase confined near L ~5.2–5.4. These findings strongly suggest that the premidnight arc is connected to highly localized pressure gradients embedded in the near-tail R2 source region via the local upward FAC.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
937836; NAS5-01072; NNX12AJ52G; NAS5-02099; GEO/ATM-110433; AC52-06NA25396
OSTI ID:
1236775
Report Number(s):
LA-UR-15-27239
Journal Information:
Journal of Geophysical Research. Space Physics, Vol. 120, Issue 10; ISSN 2169-9380
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 20 works
Citation information provided by
Web of Science

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Cited By (4)

Quiescent Discrete Auroral Arcs: A Review of Magnetospheric Generator Mechanisms journal December 2019
Quiet, Discrete Auroral Arcs—Observations journal February 2020
Recent Advancements and Remaining Challenges Associated With Inner Magnetosphere Cross‐Energy/Population Interactions (IMCEPI) journal February 2019
Revisiting substorm events with preonset aurora journal January 2018

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