Irregular structures of the F layer at high latitudes during ionospheric heating.
Results on heating the ionospheric F region above Tromsø, Norway are presented. The ionosphere was monitored by satellite tomography and amplitude scintillation methods as well as the EISCAT incoherent scatter radar. No effect of heating was observed in the daytime. In the evening and in the pre-mid...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
European Geophysical Society
2000
|
Subjects: | |
Online Access: | https://hdl.handle.net/10037/560 |
_version_ | 1829307763299188736 |
---|---|
author | Rietveld, Michael T. Tereshchenko, E.D. Kozlova, M.O. Brekke, Asgeir Evstafiev, O.V. Khudukon, B.Z. Nygren, T. |
author_facet | Rietveld, Michael T. Tereshchenko, E.D. Kozlova, M.O. Brekke, Asgeir Evstafiev, O.V. Khudukon, B.Z. Nygren, T. |
author_sort | Rietveld, Michael T. |
collection | University of Tromsø: Munin Open Research Archive |
description | Results on heating the ionospheric F region above Tromsø, Norway are presented. The ionosphere was monitored by satellite tomography and amplitude scintillation methods as well as the EISCAT incoherent scatter radar. No effect of heating was observed in the daytime. In the evening and in the pre-midnight sector, noticeable tilts of the F region were observed during heating periods. The tilts overlapped the heating cone, where the electron density decreased and irregularities exceeding 10 km in size appeared. Between the heating periods the F layer was restored to its horizontal shape. The anisotropic parameters of small-scale irregularities with scale lengths of hundreds of metres were also determined. It was found that the perpendicular anisotropy points in the direction of F region plasma flow. In some cases the results can be explained by assuming that the small-scale irregularities were generated within the heating cone and drifted out of the heating region where they were subsequently observed. |
format | Article in Journal/Newspaper |
genre | EISCAT Tromsø |
genre_facet | EISCAT Tromsø |
geographic | Norway Tromsø |
geographic_facet | Norway Tromsø |
id | ftunivtroemsoe:oai:munin.uit.no:10037/560 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_relation | Annales Geophysicae 18(2000), pp 1197-1209 https://hdl.handle.net/10037/560 |
op_rights | openAccess |
publishDate | 2000 |
publisher | European Geophysical Society |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/560 2025-04-13T14:18:07+00:00 Irregular structures of the F layer at high latitudes during ionospheric heating. Rietveld, Michael T. Tereshchenko, E.D. Kozlova, M.O. Brekke, Asgeir Evstafiev, O.V. Khudukon, B.Z. Nygren, T. 2000 909282 bytes application/pdf https://hdl.handle.net/10037/560 eng eng European Geophysical Society Annales Geophysicae 18(2000), pp 1197-1209 https://hdl.handle.net/10037/560 openAccess ionosphere active experiments auroral ionosphere ionosphere irregularities VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 Journal article Peer reviewed Tidsskriftartikkel 2000 ftunivtroemsoe 2025-03-14T05:17:55Z Results on heating the ionospheric F region above Tromsø, Norway are presented. The ionosphere was monitored by satellite tomography and amplitude scintillation methods as well as the EISCAT incoherent scatter radar. No effect of heating was observed in the daytime. In the evening and in the pre-midnight sector, noticeable tilts of the F region were observed during heating periods. The tilts overlapped the heating cone, where the electron density decreased and irregularities exceeding 10 km in size appeared. Between the heating periods the F layer was restored to its horizontal shape. The anisotropic parameters of small-scale irregularities with scale lengths of hundreds of metres were also determined. It was found that the perpendicular anisotropy points in the direction of F region plasma flow. In some cases the results can be explained by assuming that the small-scale irregularities were generated within the heating cone and drifted out of the heating region where they were subsequently observed. Article in Journal/Newspaper EISCAT Tromsø University of Tromsø: Munin Open Research Archive Norway Tromsø |
spellingShingle | ionosphere active experiments auroral ionosphere ionosphere irregularities VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 Rietveld, Michael T. Tereshchenko, E.D. Kozlova, M.O. Brekke, Asgeir Evstafiev, O.V. Khudukon, B.Z. Nygren, T. Irregular structures of the F layer at high latitudes during ionospheric heating. |
title | Irregular structures of the F layer at high latitudes during ionospheric heating. |
title_full | Irregular structures of the F layer at high latitudes during ionospheric heating. |
title_fullStr | Irregular structures of the F layer at high latitudes during ionospheric heating. |
title_full_unstemmed | Irregular structures of the F layer at high latitudes during ionospheric heating. |
title_short | Irregular structures of the F layer at high latitudes during ionospheric heating. |
title_sort | irregular structures of the f layer at high latitudes during ionospheric heating. |
topic | ionosphere active experiments auroral ionosphere ionosphere irregularities VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 |
topic_facet | ionosphere active experiments auroral ionosphere ionosphere irregularities VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 |
url | https://hdl.handle.net/10037/560 |