| Earth, Planets and Space | 卷:72 |
| Relative contributions of large-scale and wedgelet currents in the substorm current wedge | |
| L. R. Lyons1  J. M. Weygand2  V. Angelopoulos2  Y. Nishimura3  E. F. Donovan4  C. Gabrielse5  | |
| [1] Department of Atmospheric and Oceanic Sciences, University of California; | |
| [2] Department of Earth, Planetary and Space Sciences, University of California; | |
| [3] Department of Electrical and Computer Engineering and Center for Space Physics, Boston University; | |
| [4] Department of Physics and Astronomy, University of Calgary; | |
| [5] The Aerospace Corporation; | |
| 关键词: Substorm current wedge (SCW); Field-aligned current (FAC); Westward traveling surge (WTS); Plasma sheet; Bursty bulk flow (BBF); | |
| DOI : 10.1186/s40623-020-01234-x | |
| 来源: DOAJ | |
【 摘 要 】
Abstract We examined how much large-scale and localized upward and downward currents contribute to the substorm current wedge (SCW), and how they evolve over time, using the THEMIS all-sky imagers (ASIs) and ground magnetometers. One type of events is dominated by a single large-scale wedge, with upward currents over the surge and broad downward currents poleward-eastward of the surge. The other type of events is a composite of large-scale wedge and wedgelets associated with streamers, with each wedgelet having comparable intensity to the large-scale wedge currents. Among 17 auroral substorms with wide ASI coverage, the composite current type is more frequent than the single large-scale wedge type. The dawn–dusk size of each wedgelet is ~ 600 km in the ionosphere (~ 3.2 R E in the magnetotail, comparable to the flow channel size). We suggest that substorms have more than one type of SCW, and the composite current type is more frequent.
【 授权许可】
Unknown