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Substorm evolution of auroral structures

Substorm evolution of auroral structures
Substorm evolution of auroral structures
Auroral arcs are often associated with magnetically quiet time and substorm growth phases. We have studied the evolution of auroral structures during global and local magnetic activity to investigate the occurrence rate of auroral arcs during different levels of magnetic activity. The ground-magnetic and auroral conditions are described by the magnetometer and auroral camera data from five Magnetometers — Ionospheric radars — All-sky cameras Large Experiment stations in Finnish and Swedish Lapland. We identified substorm growth, expansion, and recovery phases from the local electrojet index (IL) in 1996–2007 and analyzed the auroral structures during the different phases. Auroral structures were also analyzed during different global magnetic activity levels, as described by the planetary Kp index. The distribution of auroral structures for all substorm phases and Kp levels is of similar shape. About one third of all detected structures are auroral arcs. This suggests that auroral arcs occur in all conditions as the main element of the aurora. The most arc-dominated substorm phases occur in the premidnight sector, while the least arc-dominated substorm phases take place in the dawn sector. Arc event lifetimes and expectation times calculated for different substorm phases show that the longest arc-dominated periods are found during growth phases, while the longest arc waiting times occur during expansion phases. Most of the arc events end when arcs evolve to more complex structures. This is true for all substorm phases. Based on the number of images of auroral arcs and the durations of substorm phases, we conclude that a randomly selected auroral arc most likely belongs to a substorm expansion phase. A small time delay, of the order of a minute, is observed between the magnetic signature of the substorm onset (i.e., the beginning of the negative bay) and the auroral breakup (i.e., the growth phase arc changing into a dynamic display). The magnetic onset was observed to precede the structural change in the auroral display. A longer delay of a few minutes was found between the beginning of the growth phase and the first detected auroral structure.
2169-9380
5958-5972
Partamies, Noora
7219021b-a268-41eb-8e75-80550b7cf78f
Juusola, Liisa
f5728e97-a0e0-42ee-af6e-244687f35bf9
Whiter, Daniel
9a30d7b6-ea41-44fb-bd52-3ff1964eca5c
Kauristie, Kirsti
6c818f17-8fe5-4911-9c62-055ae136d88d
Partamies, Noora
7219021b-a268-41eb-8e75-80550b7cf78f
Juusola, Liisa
f5728e97-a0e0-42ee-af6e-244687f35bf9
Whiter, Daniel
9a30d7b6-ea41-44fb-bd52-3ff1964eca5c
Kauristie, Kirsti
6c818f17-8fe5-4911-9c62-055ae136d88d

Partamies, Noora, Juusola, Liisa, Whiter, Daniel and Kauristie, Kirsti (2015) Substorm evolution of auroral structures. Journal of Geophysical Research: Space Physics, 120 (7), 5958-5972. (doi:10.1002/2015JA021217).

Record type: Article

Abstract

Auroral arcs are often associated with magnetically quiet time and substorm growth phases. We have studied the evolution of auroral structures during global and local magnetic activity to investigate the occurrence rate of auroral arcs during different levels of magnetic activity. The ground-magnetic and auroral conditions are described by the magnetometer and auroral camera data from five Magnetometers — Ionospheric radars — All-sky cameras Large Experiment stations in Finnish and Swedish Lapland. We identified substorm growth, expansion, and recovery phases from the local electrojet index (IL) in 1996–2007 and analyzed the auroral structures during the different phases. Auroral structures were also analyzed during different global magnetic activity levels, as described by the planetary Kp index. The distribution of auroral structures for all substorm phases and Kp levels is of similar shape. About one third of all detected structures are auroral arcs. This suggests that auroral arcs occur in all conditions as the main element of the aurora. The most arc-dominated substorm phases occur in the premidnight sector, while the least arc-dominated substorm phases take place in the dawn sector. Arc event lifetimes and expectation times calculated for different substorm phases show that the longest arc-dominated periods are found during growth phases, while the longest arc waiting times occur during expansion phases. Most of the arc events end when arcs evolve to more complex structures. This is true for all substorm phases. Based on the number of images of auroral arcs and the durations of substorm phases, we conclude that a randomly selected auroral arc most likely belongs to a substorm expansion phase. A small time delay, of the order of a minute, is observed between the magnetic signature of the substorm onset (i.e., the beginning of the negative bay) and the auroral breakup (i.e., the growth phase arc changing into a dynamic display). The magnetic onset was observed to precede the structural change in the auroral display. A longer delay of a few minutes was found between the beginning of the growth phase and the first detected auroral structure.

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More information

Accepted/In Press date: 19 June 2015
e-pub ahead of print date: 25 June 2015
Published date: 22 July 2015
Organisations: Astronomy Group

Identifiers

Local EPrints ID: 397224
URI: http://eprints.soton.ac.uk/id/eprint/397224
ISSN: 2169-9380
PURE UUID: b59a0e43-3aa8-4673-a5df-e89f178cf844
ORCID for Daniel Whiter: ORCID iD orcid.org/0000-0001-7130-232X

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Date deposited: 22 Jun 2016 13:20
Last modified: 15 Mar 2024 03:31

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Contributors

Author: Noora Partamies
Author: Liisa Juusola
Author: Daniel Whiter ORCID iD
Author: Kirsti Kauristie

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