Occurrence statistics of magnetic impulsive events

In this study, we perform a statistical investigation of magnetic impulse events identified in the Greenland magnetometer stations through the years 1995–2001. We focus on occurrence statistics that can be determined reliably with an automatic event identification procedure. Durin the first two year...

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Published in:Annales Geophysicae
Main Authors: T. Moretto, D. G. Sibeck, J. F. Watermann
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-22-585-2004
https://doaj.org/article/d034f03317584a11b64ab4a0ba61aeb4
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spelling ftdoajarticles:oai:doaj.org/article:d034f03317584a11b64ab4a0ba61aeb4 2023-05-15T16:28:22+02:00 Occurrence statistics of magnetic impulsive events T. Moretto D. G. Sibeck J. F. Watermann 2004-01-01T00:00:00Z https://doi.org/10.5194/angeo-22-585-2004 https://doaj.org/article/d034f03317584a11b64ab4a0ba61aeb4 EN eng Copernicus Publications https://www.ann-geophys.net/22/585/2004/angeo-22-585-2004.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-22-585-2004 0992-7689 1432-0576 https://doaj.org/article/d034f03317584a11b64ab4a0ba61aeb4 Annales Geophysicae, Vol 22, Pp 585-602 (2004) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2004 ftdoajarticles https://doi.org/10.5194/angeo-22-585-2004 2022-12-31T13:31:23Z In this study, we perform a statistical investigation of magnetic impulse events identified in the Greenland magnetometer stations through the years 1995–2001. We focus on occurrence statistics that can be determined reliably with an automatic event identification procedure. Durin the first two years we observed almost 40% more events than in the following years. Season is not a significant factor in event occurrence. Event occurrence peaks near 12:00UT, corresponding to approximately 10:00 magnetic local time (MLT) at the west coast of Greenland. More events occur prior to local noon than after. Event days are not distributed evenly. Large amplitude events, particularly, tend to appear on consecutive days. Events are observed at lower latitudes at earlier local times in a way consistent with the projection of the outer magnetospheric boundary into the ionosphere. Event latitude depends on dipole tilt angle in a manner similar to that reported for the cusp. Events occur during intervals of enhanced K p . The main reason for this is that the events themselves contribute to the K p index. Events exhibit a preference for high solar wind velocity. In particular, the large amplitude events occur during high-speed streams. A slight preference for lower density and more radial interplanetary magnetic fields, as compared to the nominal solar wind distribution, is also observed. However, both the nominal solar wind and event distribution exhibit large differences from year to year, indicating that events occur under a broad range of conditions. Key words. Ionosphere (ionospheric disturbances) Magnetospheric physics (magnetosphere-ionosphere interactions; solar wind-magnetosphere interactions) Article in Journal/Newspaper Greenland Directory of Open Access Journals: DOAJ Articles Greenland Annales Geophysicae 22 2 585 602
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
T. Moretto
D. G. Sibeck
J. F. Watermann
Occurrence statistics of magnetic impulsive events
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description In this study, we perform a statistical investigation of magnetic impulse events identified in the Greenland magnetometer stations through the years 1995–2001. We focus on occurrence statistics that can be determined reliably with an automatic event identification procedure. Durin the first two years we observed almost 40% more events than in the following years. Season is not a significant factor in event occurrence. Event occurrence peaks near 12:00UT, corresponding to approximately 10:00 magnetic local time (MLT) at the west coast of Greenland. More events occur prior to local noon than after. Event days are not distributed evenly. Large amplitude events, particularly, tend to appear on consecutive days. Events are observed at lower latitudes at earlier local times in a way consistent with the projection of the outer magnetospheric boundary into the ionosphere. Event latitude depends on dipole tilt angle in a manner similar to that reported for the cusp. Events occur during intervals of enhanced K p . The main reason for this is that the events themselves contribute to the K p index. Events exhibit a preference for high solar wind velocity. In particular, the large amplitude events occur during high-speed streams. A slight preference for lower density and more radial interplanetary magnetic fields, as compared to the nominal solar wind distribution, is also observed. However, both the nominal solar wind and event distribution exhibit large differences from year to year, indicating that events occur under a broad range of conditions. Key words. Ionosphere (ionospheric disturbances) Magnetospheric physics (magnetosphere-ionosphere interactions; solar wind-magnetosphere interactions)
format Article in Journal/Newspaper
author T. Moretto
D. G. Sibeck
J. F. Watermann
author_facet T. Moretto
D. G. Sibeck
J. F. Watermann
author_sort T. Moretto
title Occurrence statistics of magnetic impulsive events
title_short Occurrence statistics of magnetic impulsive events
title_full Occurrence statistics of magnetic impulsive events
title_fullStr Occurrence statistics of magnetic impulsive events
title_full_unstemmed Occurrence statistics of magnetic impulsive events
title_sort occurrence statistics of magnetic impulsive events
publisher Copernicus Publications
publishDate 2004
url https://doi.org/10.5194/angeo-22-585-2004
https://doaj.org/article/d034f03317584a11b64ab4a0ba61aeb4
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Annales Geophysicae, Vol 22, Pp 585-602 (2004)
op_relation https://www.ann-geophys.net/22/585/2004/angeo-22-585-2004.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-22-585-2004
0992-7689
1432-0576
https://doaj.org/article/d034f03317584a11b64ab4a0ba61aeb4
op_doi https://doi.org/10.5194/angeo-22-585-2004
container_title Annales Geophysicae
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container_issue 2
container_start_page 585
op_container_end_page 602
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