Geotail measurements compared with the motions of high-latitude auroral boundaries during two substorms

Journal Article · Thu May 01 04:00:00 EDT 1997 · Journal of Geophysical Research

DOI:https://doi.org/10.1029/97JA00307· OSTI ID:526884

Maynard, N C ^[1]; Burke, W J ^[2]; Erickson, G M ^[3]; Nakamura, M ^[4]; Mukai, T ^[5]; Kokubun, S ^[6]; Yamamoto, T ^[7]; Jacobsen, B; Egeland, A ^[8]; Samson, J C ^[9]; Weimer, D R ^[1]; Reeves, G D ^[10]; Luehr, H ^[11]

---

1. Mission Research Corporation, Nashua, New Hampshire (United States)
2. Phillips Laboratory, Hansom Air Force Base, Massachusetts (United States)
3. Center for Space Physics, Boston University, Boston, Massachusetts (United States)
4. Department of Earth and Planetary Physics, University of Tokyo, Tokyo (Japan)
5. Institute of Space and Astronautical Science, Sagamihara (Japan)
6. Solar Terrestrial Environment Laboratory, Nagoya University, Toyokawa (Japan)
7. Institute of Space and Astronautical Science, Kanagawa (Japan)
8. Department of Physics, University of Oslo, Oslo (Norway)
9. Department of Physics, Canadian Network for Space Research, University of Alberta, Edmonton, Alberta (Canada)
10. Astrophysics and Radiation Measurements, Los Alamos National Laboratory, Los Alamos, New Mexico (United States)
11. Institut fuer Geophysik und Meteorologie, Technical University of Braunschweig (Germany)

Geotail plasma and field measurements at {minus}95 R{sub E} are compared with extensive ground-based, near-Earth, and geosynchronous measurements to study relationships between auroral activity and magnetotail dynamics during the expansion phases of two substorms. The studied intervals are representative of intermittent, moderate activity. The behavior of the aurora and the observed effects at Geotail for both events are harmonized by the concept of the activation of near-Earth X lines (NEXL) after substorm onsets with subsequent discharges of one or more plasmoids down the magnetotail. The plasmoids must be viewed as three-dimensional structures which are spatially limited in the dawn-dusk direction. Also, reconnection at the NEXL must proceed at variable rates on closed magnetic field lines for significant times before beginning to reconnect lobe flux. This implies that the plasma sheet in the near-Earth magnetotail is relatively thick in comparison with an embedded current sheet and that both the NEXL and distant X line can be active simultaneously. Until reconnection at the NEXL engages lobe flux, the distant X line maintains control of the poleward auroral boundary. If the NEXL remains active after reaching the lobe, the auroral boundary can move poleward explosively. The dynamics of high-latitude aurora in the midnight region thus provides a means for monitoring these processes and indicating when significant lobe flux reconnects at the NEXL.{copyright} 1997 American Geophysical Union

• OSTI ID: 526884
• Journal Information: Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: A5 Vol. 102; ISSN JGREA2; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

66 PHYSICS
AURORAE
EARTH MAGNETOSPHERE
IONOSPHERE
MAGNETIC STORMS
MAGNETOTAIL
PLASMA SHEATH
PLASMOIDS