A possible mechanism for the formation of an eastward moving auroral spiral

The generation process of auroral spirals is described by different theories varying for their morphology and surrounding conditions. Here, a possible mechanism is proposed for an eastward moving auroral spiral, which was observed in Tromsø, Norway, during the expansion phase of a substorm on 18 Sep...

Full description

Bibliographic Details
Published in:Frontiers in Astronomy and Space Sciences
Main Authors: Maetschke, Katharina N., Kronberg, Elena A., Partamies, Noora, Grigorenko, Elena E.
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2023
Subjects:
Online Access:http://dx.doi.org/10.3389/fspas.2023.1240081
https://www.frontiersin.org/articles/10.3389/fspas.2023.1240081/full
id crfrontiers:10.3389/fspas.2023.1240081
record_format openpolar
spelling crfrontiers:10.3389/fspas.2023.1240081 2024-09-30T14:45:10+00:00 A possible mechanism for the formation of an eastward moving auroral spiral Maetschke, Katharina N. Kronberg, Elena A. Partamies, Noora Grigorenko, Elena E. 2023 http://dx.doi.org/10.3389/fspas.2023.1240081 https://www.frontiersin.org/articles/10.3389/fspas.2023.1240081/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Astronomy and Space Sciences volume 10 ISSN 2296-987X journal-article 2023 crfrontiers https://doi.org/10.3389/fspas.2023.1240081 2024-09-03T04:05:45Z The generation process of auroral spirals is described by different theories varying for their morphology and surrounding conditions. Here, a possible mechanism is proposed for an eastward moving auroral spiral, which was observed in Tromsø, Norway, during the expansion phase of a substorm on 18 September 2013. Measurements from the THEMIS-A and Cluster spacecraft were analyzed, which were located up to ∼10 R E duskward from the spiral generator region in the magnetosphere. Precursory to the spiral observation, concurrent magnetic field dipolarizations, flow bursts and electron injections were measured by the Cluster satellites between 13.6 and 14.2 R E radial distance from Earth. A local Kelvin-Helmholtz-like vortex street in the magnetic field was detected at the same time, which was likely caused by bursty bulk flows. The vortex street was oriented approximately in the X-Y (GSE) plane and presumably propagated towards the source region of the spiral due to a high dawnward velocity component in the flow bursts. The observations suggest that the spiral can have been generated by an associated vortex in the magnetotail and then mapped along the magnetic field lines to the ionosphere. To better understand the role of the ionosphere in auroral spiral generation, in future more mesoscale observations are required. Article in Journal/Newspaper Tromsø Frontiers (Publisher) Norway Tromsø Frontiers in Astronomy and Space Sciences 10
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description The generation process of auroral spirals is described by different theories varying for their morphology and surrounding conditions. Here, a possible mechanism is proposed for an eastward moving auroral spiral, which was observed in Tromsø, Norway, during the expansion phase of a substorm on 18 September 2013. Measurements from the THEMIS-A and Cluster spacecraft were analyzed, which were located up to ∼10 R E duskward from the spiral generator region in the magnetosphere. Precursory to the spiral observation, concurrent magnetic field dipolarizations, flow bursts and electron injections were measured by the Cluster satellites between 13.6 and 14.2 R E radial distance from Earth. A local Kelvin-Helmholtz-like vortex street in the magnetic field was detected at the same time, which was likely caused by bursty bulk flows. The vortex street was oriented approximately in the X-Y (GSE) plane and presumably propagated towards the source region of the spiral due to a high dawnward velocity component in the flow bursts. The observations suggest that the spiral can have been generated by an associated vortex in the magnetotail and then mapped along the magnetic field lines to the ionosphere. To better understand the role of the ionosphere in auroral spiral generation, in future more mesoscale observations are required.
format Article in Journal/Newspaper
author Maetschke, Katharina N.
Kronberg, Elena A.
Partamies, Noora
Grigorenko, Elena E.
spellingShingle Maetschke, Katharina N.
Kronberg, Elena A.
Partamies, Noora
Grigorenko, Elena E.
A possible mechanism for the formation of an eastward moving auroral spiral
author_facet Maetschke, Katharina N.
Kronberg, Elena A.
Partamies, Noora
Grigorenko, Elena E.
author_sort Maetschke, Katharina N.
title A possible mechanism for the formation of an eastward moving auroral spiral
title_short A possible mechanism for the formation of an eastward moving auroral spiral
title_full A possible mechanism for the formation of an eastward moving auroral spiral
title_fullStr A possible mechanism for the formation of an eastward moving auroral spiral
title_full_unstemmed A possible mechanism for the formation of an eastward moving auroral spiral
title_sort possible mechanism for the formation of an eastward moving auroral spiral
publisher Frontiers Media SA
publishDate 2023
url http://dx.doi.org/10.3389/fspas.2023.1240081
https://www.frontiersin.org/articles/10.3389/fspas.2023.1240081/full
geographic Norway
Tromsø
geographic_facet Norway
Tromsø
genre Tromsø
genre_facet Tromsø
op_source Frontiers in Astronomy and Space Sciences
volume 10
ISSN 2296-987X
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fspas.2023.1240081
container_title Frontiers in Astronomy and Space Sciences
container_volume 10
_version_ 1811646000766386176