A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ
Abstract Volcanic plumes generate lightning from the electrification of plume particles. Volcanic plume charging at over 1200 km from its source was observed from in situ balloon sampling of the April 2010 Eyjafjallajökull plume over Scotland. Whilst upper and lower edge charging of a horizontal plu...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1054.4512 2023-05-15T16:09:29+02:00 A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ R G Harrison K A Nicoll Z Ulanowski T A Mather The Pennsylvania State University CiteSeerX Archives 2010 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1054.4512 http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1054.4512 http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf text 2010 ftciteseerx 2020-04-12T00:19:48Z Abstract Volcanic plumes generate lightning from the electrification of plume particles. Volcanic plume charging at over 1200 km from its source was observed from in situ balloon sampling of the April 2010 Eyjafjallajökull plume over Scotland. Whilst upper and lower edge charging of a horizontal plume is expected from fair weather atmospheric electricity, the plume over Scotland showed sustained positive charge well beneath the upper plume edge. At these distances from the source, the charging cannot be a remnant of the eruption itself because of charge relaxation in the finite conductivity of atmospheric air. Text Eyjafjallajökull Unknown |
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English |
description |
Abstract Volcanic plumes generate lightning from the electrification of plume particles. Volcanic plume charging at over 1200 km from its source was observed from in situ balloon sampling of the April 2010 Eyjafjallajökull plume over Scotland. Whilst upper and lower edge charging of a horizontal plume is expected from fair weather atmospheric electricity, the plume over Scotland showed sustained positive charge well beneath the upper plume edge. At these distances from the source, the charging cannot be a remnant of the eruption itself because of charge relaxation in the finite conductivity of atmospheric air. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R G Harrison K A Nicoll Z Ulanowski T A Mather |
spellingShingle |
R G Harrison K A Nicoll Z Ulanowski T A Mather A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
author_facet |
R G Harrison K A Nicoll Z Ulanowski T A Mather |
author_sort |
R G Harrison |
title |
A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
title_short |
A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
title_full |
A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
title_fullStr |
A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
title_full_unstemmed |
A.: Self-charging of the Eyjafjallajökull volcanic ash plume, Environ |
title_sort |
a.: self-charging of the eyjafjallajökull volcanic ash plume, environ |
publishDate |
2010 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1054.4512 http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf |
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Eyjafjallajökull |
genre_facet |
Eyjafjallajökull |
op_source |
http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1054.4512 http://controverses.mines-paristech.fr/public/promo10/promo10_G11/data/documents/1748-9326_5_2_024004.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766405369200902144 |