Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times
During periods of increased magnetospheric activity, whistler wave emissions have been observed with increased wave amplitudes. We consider a pitch angle diffusion mechanism that is shown to scale with whistler wave amplitude and hence is 'switched on' during these periods of intense activ...
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ESA PUBLICATIONS DIVISION C/O ESTEC
2000
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ftuwarwick:oai:wrap.warwick.ac.uk:11432 2023-05-15T14:26:05+02:00 Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times Wilson, A 2000 http://wrap.warwick.ac.uk/11432/ unknown ESA PUBLICATIONS DIVISION C/O ESTEC UNSPECIFIED (2000) Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times. In: 5th International Conference on Substorms, ARCTIC & ANTARCTIC RES INST CONGRESS CTR, ST PETERSBURG, RUSSIA, MAY 16-20, 2000. Published in: PROCEEDINGS OF THE FIFTH INTERNATIONAL CONFERENCE ON SUBSTORMS, 443 pp. 217-220. ISBN 92-9092-772-0. ISSN 0379-6566. QB Astronomy Conference Item NonPeerReviewed 2000 ftuwarwick 2022-03-16T20:08:39Z During periods of increased magnetospheric activity, whistler wave emissions have been observed with increased wave amplitudes. We consider a pitch angle diffusion mechanism that is shown to scale with whistler wave amplitude and hence is 'switched on' during these periods of intense activity. We consider the interaction between relativistic electrons and two oppositely directed, parallel propagating whistler mode waves. We show that for intense whistlers this process is stochastic and results in strong electron pitch angle diffusion. We show that the interaction is rapid, occur on timescales of the order of tens of electron gyroperiods and that the interaction is sensitive to wave amplitude, wave frequency and electron energy. Conference Object Arctic The University of Warwick: WRAP - Warwick Research Archive Portal |
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The University of Warwick: WRAP - Warwick Research Archive Portal |
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ftuwarwick |
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unknown |
topic |
QB Astronomy |
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QB Astronomy Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
topic_facet |
QB Astronomy |
description |
During periods of increased magnetospheric activity, whistler wave emissions have been observed with increased wave amplitudes. We consider a pitch angle diffusion mechanism that is shown to scale with whistler wave amplitude and hence is 'switched on' during these periods of intense activity. We consider the interaction between relativistic electrons and two oppositely directed, parallel propagating whistler mode waves. We show that for intense whistlers this process is stochastic and results in strong electron pitch angle diffusion. We show that the interaction is rapid, occur on timescales of the order of tens of electron gyroperiods and that the interaction is sensitive to wave amplitude, wave frequency and electron energy. |
author2 |
Wilson, A |
format |
Conference Object |
title |
Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
title_short |
Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
title_full |
Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
title_fullStr |
Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
title_full_unstemmed |
Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
title_sort |
enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times |
publisher |
ESA PUBLICATIONS DIVISION C/O ESTEC |
publishDate |
2000 |
url |
http://wrap.warwick.ac.uk/11432/ |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
UNSPECIFIED (2000) Enhanced pitch angle diffusion due to electron-whistler interactions during disturbed times. In: 5th International Conference on Substorms, ARCTIC & ANTARCTIC RES INST CONGRESS CTR, ST PETERSBURG, RUSSIA, MAY 16-20, 2000. Published in: PROCEEDINGS OF THE FIFTH INTERNATIONAL CONFERENCE ON SUBSTORMS, 443 pp. 217-220. ISBN 92-9092-772-0. ISSN 0379-6566. |
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1766298563173679104 |