DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND
We discuss substorm observations made near 2100 magnetic local time (MLT) on March 7, 1991, in a collaborative study involving data from the European Incoherent Scatter radar, all-sky camera data, and magnetometer data from the Tromso Auroral Observatory, the U.K. Sub-Auroral Magnetometer Network (S...
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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AMER GEOPHYSICAL UNION
1995
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Online Access: | http://discovery.ucl.ac.uk/100146/ |
_version_ | 1821571515527725056 |
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author | GAZEY, NGJ LOCKWOOD, M SMITH, PN COLES, S BUNTING, RJ LESTER, M AYLWARD, AD YEOMAN, TK LUHR, H |
author_facet | GAZEY, NGJ LOCKWOOD, M SMITH, PN COLES, S BUNTING, RJ LESTER, M AYLWARD, AD YEOMAN, TK LUHR, H |
author_sort | GAZEY, NGJ |
collection | University College London: UCL Discovery |
description | We discuss substorm observations made near 2100 magnetic local time (MLT) on March 7, 1991, in a collaborative study involving data from the European Incoherent Scatter radar, all-sky camera data, and magnetometer data from the Tromso Auroral Observatory, the U.K. Sub-Auroral Magnetometer Network (SAMNET) and the IMAGE magnetometer chain. We conclude that for the substorm studied a plasmoid was not pinched off until at least 10 min after onset-at the local time of the observations (2100 MLT) and that the main substorm electrojet expanded westward over this local time 14 min after onset. In the late growth phase/early expansion phase, we observed southward drifting arcs probably moving faster than the background plasma. Similar southward moving arcs in the recovery phase moved at a speed which does not appear to be significantly different from the measured plasma flow speed. We discuss these data in terms of the ''Kiruna conjecture'' and classical ''near-Earth neutral line'' paradigms, since the data show features of both models of substorm development. We suggest that longitudinal variation in behavior may reconcile the differences between the two models in the case of this substorm. |
format | Article in Journal/Newspaper |
genre | Kiruna Tromso Tromso |
genre_facet | Kiruna Tromso Tromso |
geographic | Kiruna Tromso |
geographic_facet | Kiruna Tromso |
id | ftucl:oai:eprints.ucl.ac.uk.OAI2:100146 |
institution | Open Polar |
language | unknown |
long_lat | ENVELOPE(16.546,16.546,68.801,68.801) |
op_collection_id | ftucl |
op_source | J GEOPHYS RES-SPACE , 100 (A6) 9633 - 9648. (1995) |
publishDate | 1995 |
publisher | AMER GEOPHYSICAL UNION |
record_format | openpolar |
spelling | ftucl:oai:eprints.ucl.ac.uk.OAI2:100146 2025-01-16T22:54:46+00:00 DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND GAZEY, NGJ LOCKWOOD, M SMITH, PN COLES, S BUNTING, RJ LESTER, M AYLWARD, AD YEOMAN, TK LUHR, H 1995-06-01 http://discovery.ucl.ac.uk/100146/ unknown AMER GEOPHYSICAL UNION J GEOPHYS RES-SPACE , 100 (A6) 9633 - 9648. (1995) MAGNETIC-FIELD AURORAL ARCS GROWTH-PHASE NIGHTSIDE MAGNETOSPHERE MHD SIMULATIONS ELECTRIC-FIELDS PLASMA SHEET RECONNECTION MAGNETOTAIL EXPANSION Article 1995 ftucl 2016-01-15T02:33:15Z We discuss substorm observations made near 2100 magnetic local time (MLT) on March 7, 1991, in a collaborative study involving data from the European Incoherent Scatter radar, all-sky camera data, and magnetometer data from the Tromso Auroral Observatory, the U.K. Sub-Auroral Magnetometer Network (SAMNET) and the IMAGE magnetometer chain. We conclude that for the substorm studied a plasmoid was not pinched off until at least 10 min after onset-at the local time of the observations (2100 MLT) and that the main substorm electrojet expanded westward over this local time 14 min after onset. In the late growth phase/early expansion phase, we observed southward drifting arcs probably moving faster than the background plasma. Similar southward moving arcs in the recovery phase moved at a speed which does not appear to be significantly different from the measured plasma flow speed. We discuss these data in terms of the ''Kiruna conjecture'' and classical ''near-Earth neutral line'' paradigms, since the data show features of both models of substorm development. We suggest that longitudinal variation in behavior may reconcile the differences between the two models in the case of this substorm. Article in Journal/Newspaper Kiruna Tromso Tromso University College London: UCL Discovery Kiruna Tromso ENVELOPE(16.546,16.546,68.801,68.801) |
spellingShingle | MAGNETIC-FIELD AURORAL ARCS GROWTH-PHASE NIGHTSIDE MAGNETOSPHERE MHD SIMULATIONS ELECTRIC-FIELDS PLASMA SHEET RECONNECTION MAGNETOTAIL EXPANSION GAZEY, NGJ LOCKWOOD, M SMITH, PN COLES, S BUNTING, RJ LESTER, M AYLWARD, AD YEOMAN, TK LUHR, H DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title | DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title_full | DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title_fullStr | DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title_full_unstemmed | DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title_short | DEVELOPMENT OF SUBSTORM CROSS-TAIL CURRENT DISRUPTION AS SEEN FROM THE GROUND |
title_sort | development of substorm cross-tail current disruption as seen from the ground |
topic | MAGNETIC-FIELD AURORAL ARCS GROWTH-PHASE NIGHTSIDE MAGNETOSPHERE MHD SIMULATIONS ELECTRIC-FIELDS PLASMA SHEET RECONNECTION MAGNETOTAIL EXPANSION |
topic_facet | MAGNETIC-FIELD AURORAL ARCS GROWTH-PHASE NIGHTSIDE MAGNETOSPHERE MHD SIMULATIONS ELECTRIC-FIELDS PLASMA SHEET RECONNECTION MAGNETOTAIL EXPANSION |
url | http://discovery.ucl.ac.uk/100146/ |