The cusp in rapid transition

We report on a transitional state of the Northern Hemisphere winter cusp following a strong bipolar rotation of the interplanetary magnetic field (IMF) from south to north (−20 to 20 nT in 8 min). We combine ground optical data (meridian scanning photometer and an all-sky camera at Ny Ålesund, Svalb...

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Published in:Journal of Geophysical Research: Space Physics
Main Authors: Sandholt, P. E., Farrugia, Charlie J., Moen, J., Denig, W. F.
Format: Text
Language:unknown
Published: University of New Hampshire Scholars' Repository 2002
Subjects:
Online Access:https://scholars.unh.edu/cmerg/254
https://doi.org/10.1029/2001JA009214
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spelling ftuninhampshire:oai:scholars.unh.edu:cmerg-1253 2023-05-15T17:48:28+02:00 The cusp in rapid transition Sandholt, P. E. Farrugia, Charlie J. Moen, J. Denig, W. F. 2002-12-06T08:00:00Z https://scholars.unh.edu/cmerg/254 https://doi.org/10.1029/2001JA009214 unknown University of New Hampshire Scholars' Repository https://scholars.unh.edu/cmerg/254 https://doi.org/10.1029/2001JA009214 Coronal Mass Ejection Research Group text 2002 ftuninhampshire https://doi.org/10.1029/2001JA009214 2023-01-30T22:05:14Z We report on a transitional state of the Northern Hemisphere winter cusp following a strong bipolar rotation of the interplanetary magnetic field (IMF) from south to north (−20 to 20 nT in 8 min). We combine ground optical data (meridian scanning photometer and an all-sky camera at Ny Ålesund, Svalbard (76°MLAT)) with magnetometer and particle precipitation data (ions and electrons) and ion drift observations obtained during an overpass of spacecraft DMSP F13. The isolated IMF signature (southward turning followed by northward turning) excited a specific two-phase response in the cusp ionosphere, consisting of an initial 5 min long activation of the type 1 (southward IMF) cusp aurora which was followed by a type 2 (northward IMF) aurora of similar duration, located at slighty higher latitude. The type 1 aurora persisted during this phase but at diminished intensity. The type 2 aurora was accompanied by the excitation of a double arc with very strong green line emission at the poleward boundary of the cusp. These signatures are ascribed to a rapid transition in the IMF-magnetosphere interconnection geometry, with an initial pulse of enhanced reconnection rate at subcusp latitudes being followed by an event at high latitudes. The most important findings are (1) the rapid (2 min long) transition between the two distinct cusp states, (2) the attendant excitation of discrete auroral arcs in the region of strong flow shear at the poleward boundary of the northward IMF (Bz ≫ 0; By ≫ 0) cusp, and (3) the existence of a bifurcated cusp geometry during the latter IMF condition. Text Ny Ålesund Ny-Ålesund Svalbard University of New Hampshire: Scholars Repository Svalbard Ny-Ålesund Journal of Geophysical Research: Space Physics 107 A12 SMP 8-1 SMP 8-10
institution Open Polar
collection University of New Hampshire: Scholars Repository
op_collection_id ftuninhampshire
language unknown
description We report on a transitional state of the Northern Hemisphere winter cusp following a strong bipolar rotation of the interplanetary magnetic field (IMF) from south to north (−20 to 20 nT in 8 min). We combine ground optical data (meridian scanning photometer and an all-sky camera at Ny Ålesund, Svalbard (76°MLAT)) with magnetometer and particle precipitation data (ions and electrons) and ion drift observations obtained during an overpass of spacecraft DMSP F13. The isolated IMF signature (southward turning followed by northward turning) excited a specific two-phase response in the cusp ionosphere, consisting of an initial 5 min long activation of the type 1 (southward IMF) cusp aurora which was followed by a type 2 (northward IMF) aurora of similar duration, located at slighty higher latitude. The type 1 aurora persisted during this phase but at diminished intensity. The type 2 aurora was accompanied by the excitation of a double arc with very strong green line emission at the poleward boundary of the cusp. These signatures are ascribed to a rapid transition in the IMF-magnetosphere interconnection geometry, with an initial pulse of enhanced reconnection rate at subcusp latitudes being followed by an event at high latitudes. The most important findings are (1) the rapid (2 min long) transition between the two distinct cusp states, (2) the attendant excitation of discrete auroral arcs in the region of strong flow shear at the poleward boundary of the northward IMF (Bz ≫ 0; By ≫ 0) cusp, and (3) the existence of a bifurcated cusp geometry during the latter IMF condition.
format Text
author Sandholt, P. E.
Farrugia, Charlie J.
Moen, J.
Denig, W. F.
spellingShingle Sandholt, P. E.
Farrugia, Charlie J.
Moen, J.
Denig, W. F.
The cusp in rapid transition
author_facet Sandholt, P. E.
Farrugia, Charlie J.
Moen, J.
Denig, W. F.
author_sort Sandholt, P. E.
title The cusp in rapid transition
title_short The cusp in rapid transition
title_full The cusp in rapid transition
title_fullStr The cusp in rapid transition
title_full_unstemmed The cusp in rapid transition
title_sort cusp in rapid transition
publisher University of New Hampshire Scholars' Repository
publishDate 2002
url https://scholars.unh.edu/cmerg/254
https://doi.org/10.1029/2001JA009214
geographic Svalbard
Ny-Ålesund
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genre Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
op_source Coronal Mass Ejection Research Group
op_relation https://scholars.unh.edu/cmerg/254
https://doi.org/10.1029/2001JA009214
op_doi https://doi.org/10.1029/2001JA009214
container_title Journal of Geophysical Research: Space Physics
container_volume 107
container_issue A12
container_start_page SMP 8-1
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