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Article: Simultaneous Remote Observations of Intense Reconnection Effects by DMSP and MMS Spacecraft During a Storm Time Substorm
Title | Simultaneous Remote Observations of Intense Reconnection Effects by DMSP and MMS Spacecraft During a Storm Time Substorm |
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Authors | Varsani, A.Nakamura, R.Sergeev, V. A.Baumjohann, W.Owen, C. J.Petrukovich, A. A.Yao, Z.Nakamura, T. K.M.Kubyshkina, M. V.Sotirelis, T.Burch, J. L.Genestreti, K. J.Vörös, Z.Andriopoulou, M.Gershman, D. J.Avanov, L. A.Magnes, W.Russell, C. T.Plaschke, F.Khotyaintsev, Y. V.Giles, B. L.Coffey, V. N.Dorelli, J. C.Strangeway, R. J.Torbert, R. B.Lindqvist, P. A.Ergun, R. |
Keywords | magnetic reconnection Magnetospheric Multiscale (MMS) mission plasma sheet boundary layer (PSBL) |
Issue Date | 2017 |
Citation | Journal of Geophysical Research: Space Physics, 2017, v. 122, n. 11, p. 10,891-10,909 How to Cite? |
Abstract | During a magnetic storm on 23 June 2015, several very intense substorms took place, with signatures observed by multiple spacecraft including DMSP and Magnetospheric Multiscale (MMS). At the time of interest, DMSP F18 crossed inbound through a poleward expanding auroral bulge boundary at 23.5 h magnetic local time (MLT), while MMS was located duskward of 22 h MLT during an inward crossing of the expanding plasma sheet boundary. The two spacecraft observed a consistent set of signatures as they simultaneously crossed the reconnection separatrix layer during this very intense reconnection event. These include (1) energy dispersion of the energetic ions and electrons traveling earthward, accompanied with high electron energies in the vicinity of the separatrix; (2) energy dispersion of polar rain electrons, with a high-energy cutoff; and (3) intense inward convection of the magnetic field lines at the MMS location. The high temporal resolution measurements by MMS provide unprecedented observations of the outermost electron boundary layer. We discuss the relevance of the energy dispersion of the electrons, and their pitch angle distribution, to the spatial and temporal evolution of the boundary layer. The results indicate that the underlying magnetotail magnetic reconnection process was an intrinsically impulsive and the active X-line was located relatively close to the Earth, approximately at 16–18 RE. |
Persistent Identifier | http://hdl.handle.net/10722/334515 |
ISSN | 2023 Impact Factor: 2.6 2023 SCImago Journal Rankings: 0.845 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Varsani, A. | - |
dc.contributor.author | Nakamura, R. | - |
dc.contributor.author | Sergeev, V. A. | - |
dc.contributor.author | Baumjohann, W. | - |
dc.contributor.author | Owen, C. J. | - |
dc.contributor.author | Petrukovich, A. A. | - |
dc.contributor.author | Yao, Z. | - |
dc.contributor.author | Nakamura, T. K.M. | - |
dc.contributor.author | Kubyshkina, M. V. | - |
dc.contributor.author | Sotirelis, T. | - |
dc.contributor.author | Burch, J. L. | - |
dc.contributor.author | Genestreti, K. J. | - |
dc.contributor.author | Vörös, Z. | - |
dc.contributor.author | Andriopoulou, M. | - |
dc.contributor.author | Gershman, D. J. | - |
dc.contributor.author | Avanov, L. A. | - |
dc.contributor.author | Magnes, W. | - |
dc.contributor.author | Russell, C. T. | - |
dc.contributor.author | Plaschke, F. | - |
dc.contributor.author | Khotyaintsev, Y. V. | - |
dc.contributor.author | Giles, B. L. | - |
dc.contributor.author | Coffey, V. N. | - |
dc.contributor.author | Dorelli, J. C. | - |
dc.contributor.author | Strangeway, R. J. | - |
dc.contributor.author | Torbert, R. B. | - |
dc.contributor.author | Lindqvist, P. A. | - |
dc.contributor.author | Ergun, R. | - |
dc.date.accessioned | 2023-10-20T06:48:41Z | - |
dc.date.available | 2023-10-20T06:48:41Z | - |
dc.date.issued | 2017 | - |
dc.identifier.citation | Journal of Geophysical Research: Space Physics, 2017, v. 122, n. 11, p. 10,891-10,909 | - |
dc.identifier.issn | 2169-9380 | - |
dc.identifier.uri | http://hdl.handle.net/10722/334515 | - |
dc.description.abstract | During a magnetic storm on 23 June 2015, several very intense substorms took place, with signatures observed by multiple spacecraft including DMSP and Magnetospheric Multiscale (MMS). At the time of interest, DMSP F18 crossed inbound through a poleward expanding auroral bulge boundary at 23.5 h magnetic local time (MLT), while MMS was located duskward of 22 h MLT during an inward crossing of the expanding plasma sheet boundary. The two spacecraft observed a consistent set of signatures as they simultaneously crossed the reconnection separatrix layer during this very intense reconnection event. These include (1) energy dispersion of the energetic ions and electrons traveling earthward, accompanied with high electron energies in the vicinity of the separatrix; (2) energy dispersion of polar rain electrons, with a high-energy cutoff; and (3) intense inward convection of the magnetic field lines at the MMS location. The high temporal resolution measurements by MMS provide unprecedented observations of the outermost electron boundary layer. We discuss the relevance of the energy dispersion of the electrons, and their pitch angle distribution, to the spatial and temporal evolution of the boundary layer. The results indicate that the underlying magnetotail magnetic reconnection process was an intrinsically impulsive and the active X-line was located relatively close to the Earth, approximately at 16–18 RE. | - |
dc.language | eng | - |
dc.relation.ispartof | Journal of Geophysical Research: Space Physics | - |
dc.subject | magnetic reconnection | - |
dc.subject | Magnetospheric Multiscale (MMS) mission | - |
dc.subject | plasma sheet boundary layer (PSBL) | - |
dc.title | Simultaneous Remote Observations of Intense Reconnection Effects by DMSP and MMS Spacecraft During a Storm Time Substorm | - |
dc.type | Article | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.1002/2017JA024547 | - |
dc.identifier.scopus | eid_2-s2.0-85034576071 | - |
dc.identifier.volume | 122 | - |
dc.identifier.issue | 11 | - |
dc.identifier.spage | 10,891 | - |
dc.identifier.epage | 10,909 | - |
dc.identifier.eissn | 2169-9402 | - |
dc.identifier.isi | WOS:000419938600001 | - |