Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada
Observations at Inuvik (70.4° dipole latitude) have shown that supersonic motions of auroral arcs that sweep across the zenith from south to north during poleward expansions of auroral substorms do not generate observable auroral infrasonic waves. This is in contrast to the fact that equator-ward su...
Published in: | Geophysical Journal of the Royal Astronomical Society |
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1971
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fthighwire:oai:open-archive.highwire.org:gji:26/1-4/179 2023-05-15T16:55:43+02:00 Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada Wilson, Charles R. 1971-12-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/26/1-4/179 https://doi.org/10.1111/j.1365-246X.1971.tb03391.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/26/1-4/179 http://dx.doi.org/10.1111/j.1365-246X.1971.tb03391.x Copyright (C) 1971, Oxford University Press Articles TEXT 1971 fthighwire https://doi.org/10.1111/j.1365-246X.1971.tb03391.x 2016-11-16T18:49:06Z Observations at Inuvik (70.4° dipole latitude) have shown that supersonic motions of auroral arcs that sweep across the zenith from south to north during poleward expansions of auroral substorms do not generate observable auroral infrasonic waves. This is in contrast to the fact that equator-ward supersonic motions of similar auroral arcs do produce large amplitude infrasonic bow waves. These results imply an asymmetry in the basic generation mechanism of infrasound within the auroral electrojet arcs. Text Inuvik HighWire Press (Stanford University) Canada Inuvik ENVELOPE(-133.610,-133.610,68.341,68.341) Geophysical Journal of the Royal Astronomical Society 26 1-4 179 181 |
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Open Polar |
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HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
Articles |
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Articles Wilson, Charles R. Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
topic_facet |
Articles |
description |
Observations at Inuvik (70.4° dipole latitude) have shown that supersonic motions of auroral arcs that sweep across the zenith from south to north during poleward expansions of auroral substorms do not generate observable auroral infrasonic waves. This is in contrast to the fact that equator-ward supersonic motions of similar auroral arcs do produce large amplitude infrasonic bow waves. These results imply an asymmetry in the basic generation mechanism of infrasound within the auroral electrojet arcs. |
format |
Text |
author |
Wilson, Charles R. |
author_facet |
Wilson, Charles R. |
author_sort |
Wilson, Charles R. |
title |
Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
title_short |
Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
title_full |
Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
title_fullStr |
Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
title_full_unstemmed |
Auroral Infrasonic Waves and Poleward Expansions of Auroral Substorms at Inuvik, N.W.T., Canada |
title_sort |
auroral infrasonic waves and poleward expansions of auroral substorms at inuvik, n.w.t., canada |
publisher |
Oxford University Press |
publishDate |
1971 |
url |
http://gji.oxfordjournals.org/cgi/content/short/26/1-4/179 https://doi.org/10.1111/j.1365-246X.1971.tb03391.x |
long_lat |
ENVELOPE(-133.610,-133.610,68.341,68.341) |
geographic |
Canada Inuvik |
geographic_facet |
Canada Inuvik |
genre |
Inuvik |
genre_facet |
Inuvik |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/26/1-4/179 http://dx.doi.org/10.1111/j.1365-246X.1971.tb03391.x |
op_rights |
Copyright (C) 1971, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1971.tb03391.x |
container_title |
Geophysical Journal of the Royal Astronomical Society |
container_volume |
26 |
container_issue |
1-4 |
container_start_page |
179 |
op_container_end_page |
181 |
_version_ |
1766046772321320960 |