On the formation and origin of substorm growth phase/onset auroral arcs inferred from conjugate space-ground observations
- The Johns Hopkins Univ. Applied Physics Lab., Laurel, MD (United States); Nagoya Univ., Nagoya (Japan)
- The Johns Hopkins Univ. Applied Physics Lab., Laurel, MD (United States)
- New Jersey Institute of Technology, Newark, NJ (United States)
- Nagoya Univ., Nagoya (Japan)
- Athabasca Univ., Athabasca, AB (Canada)
- Univ. of Iowa, Iowa City, IA (United States)
- 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
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