Geomagnetic micropulsations with periods 0.3-3 seconds ...

The classification and possible origin of geomagnetic micropulsations are discussed. In particular, pearls are described in some detail and previous investigations reviewed. Records from Victoria and Resolute Bay, Canada; Uppsala, Sweden; Reykjavik, Iceland; Huancayo, Peru; Ruth, Nevada and Isabella...

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Main Author: Jolley, Edmund Joseph
Format: Text
Language:English
Published: University of British Columbia 2011
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0085324
https://doi.library.ubc.ca/10.14288/1.0085324
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spelling ftdatacite:10.14288/1.0085324 2024-04-28T08:25:51+00:00 Geomagnetic micropulsations with periods 0.3-3 seconds ... Jolley, Edmund Joseph 2011 https://dx.doi.org/10.14288/1.0085324 https://doi.library.ubc.ca/10.14288/1.0085324 en eng University of British Columbia article-journal Text ScholarlyArticle 2011 ftdatacite https://doi.org/10.14288/1.0085324 2024-04-02T09:33:48Z The classification and possible origin of geomagnetic micropulsations are discussed. In particular, pearls are described in some detail and previous investigations reviewed. Records from Victoria and Resolute Bay, Canada; Uppsala, Sweden; Reykjavik, Iceland; Huancayo, Peru; Ruth, Nevada and Isabella and Palomar, California are examined and the times of commencement and termination of pearl activity determined. The conclusion is reached that pearls in mid-latitudes are local mean time dependent and tend to occur during two periods of the day. These periods correspond roughly to sunrise and sunset, the times of rapid change in the critical frequency in the F₂ layer. Pearls seem to occur most often when the geomagnetic Kp index is less than 4o and greater than 0₊. No correlation is evident between occasional pearl-like signals at Huancayo and pearls observed at other stations. It is suggested that the appearance of pearls is to a certain extent controlled by local ionospheric conditions. ... Text Iceland Resolute Bay DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description The classification and possible origin of geomagnetic micropulsations are discussed. In particular, pearls are described in some detail and previous investigations reviewed. Records from Victoria and Resolute Bay, Canada; Uppsala, Sweden; Reykjavik, Iceland; Huancayo, Peru; Ruth, Nevada and Isabella and Palomar, California are examined and the times of commencement and termination of pearl activity determined. The conclusion is reached that pearls in mid-latitudes are local mean time dependent and tend to occur during two periods of the day. These periods correspond roughly to sunrise and sunset, the times of rapid change in the critical frequency in the F₂ layer. Pearls seem to occur most often when the geomagnetic Kp index is less than 4o and greater than 0₊. No correlation is evident between occasional pearl-like signals at Huancayo and pearls observed at other stations. It is suggested that the appearance of pearls is to a certain extent controlled by local ionospheric conditions. ...
format Text
author Jolley, Edmund Joseph
spellingShingle Jolley, Edmund Joseph
Geomagnetic micropulsations with periods 0.3-3 seconds ...
author_facet Jolley, Edmund Joseph
author_sort Jolley, Edmund Joseph
title Geomagnetic micropulsations with periods 0.3-3 seconds ...
title_short Geomagnetic micropulsations with periods 0.3-3 seconds ...
title_full Geomagnetic micropulsations with periods 0.3-3 seconds ...
title_fullStr Geomagnetic micropulsations with periods 0.3-3 seconds ...
title_full_unstemmed Geomagnetic micropulsations with periods 0.3-3 seconds ...
title_sort geomagnetic micropulsations with periods 0.3-3 seconds ...
publisher University of British Columbia
publishDate 2011
url https://dx.doi.org/10.14288/1.0085324
https://doi.library.ubc.ca/10.14288/1.0085324
genre Iceland
Resolute Bay
genre_facet Iceland
Resolute Bay
op_doi https://doi.org/10.14288/1.0085324
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