Plasma irregularity production in the polar cap f-region ionosphere

Dissertation (Ph.D.) University of Alaska Fairbanks, 2017 Plasma in the Earth's ionosphere is highly irregular on scales ranging between a few centimeters and hundreds of kilometers. Small-scale irregularities or plasma waves can scatter radio waves resulting in a loss of signal for navigation...

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Main Author: Lamarche, Leslie
Other Authors: Makarevich, Roman, Bristow, William, Conde, Mark, Zhang, Hui
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/11122/7619
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/7619 2023-05-15T14:02:28+02:00 Plasma irregularity production in the polar cap f-region ionosphere Lamarche, Leslie Makarevich, Roman Bristow, William Conde, Mark Zhang, Hui 2017-05 http://hdl.handle.net/11122/7619 en_US eng http://hdl.handle.net/11122/7619 Department of Physics Dissertation phd 2017 ftunivalaska 2023-02-23T21:36:52Z Dissertation (Ph.D.) University of Alaska Fairbanks, 2017 Plasma in the Earth's ionosphere is highly irregular on scales ranging between a few centimeters and hundreds of kilometers. Small-scale irregularities or plasma waves can scatter radio waves resulting in a loss of signal for navigation and communication networks. The polar region is particularly susceptible to strong disturbances due to its direct connection with the Sun's magnetic field and energetic particles. In this thesis, factors that contribute to the production of decameter-scale plasma irregularities in the polar F region ionosphere are investigated. Both global and local control of irregularity production are studied, i.e. we consider global solar control through solar illumination and solar wind as well as much more local control by plasma density gradients and convection electric field. In the first experimental study, solar control of irregularity production is investigated using the Super Dual Auroral Radar Network (SuperDARN) radar at McMurdo, Antarctica. The occurrence trends for irregularities are analyzed statistically and a model is developed that describes the location of radar echoes within the radar's field-of-view. The trends are explained through variations in background plasma density with solar illumination affecting radar beam propagation. However, it is found that the irregularity occurrence during the night is higher than expected from ray tracing simulations based on a standard ionospheric density model. The high occurrence at night implies an additional source of plasma density and it is proposed that large-scale density enhancements called polar patches may be the source of this density. Additionally, occurrence maximizes around the terminator due to different competing irregularity production processes that favor a more or less sunlit ionosphere. The second study is concerned with modeling irregularity characterics near a largescale density gradient reversal, such as those expected near polar patches, with a particular ... Doctoral or Postdoctoral Thesis Antarc* Antarctica Alaska University of Alaska: ScholarWorks@UA Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Dissertation (Ph.D.) University of Alaska Fairbanks, 2017 Plasma in the Earth's ionosphere is highly irregular on scales ranging between a few centimeters and hundreds of kilometers. Small-scale irregularities or plasma waves can scatter radio waves resulting in a loss of signal for navigation and communication networks. The polar region is particularly susceptible to strong disturbances due to its direct connection with the Sun's magnetic field and energetic particles. In this thesis, factors that contribute to the production of decameter-scale plasma irregularities in the polar F region ionosphere are investigated. Both global and local control of irregularity production are studied, i.e. we consider global solar control through solar illumination and solar wind as well as much more local control by plasma density gradients and convection electric field. In the first experimental study, solar control of irregularity production is investigated using the Super Dual Auroral Radar Network (SuperDARN) radar at McMurdo, Antarctica. The occurrence trends for irregularities are analyzed statistically and a model is developed that describes the location of radar echoes within the radar's field-of-view. The trends are explained through variations in background plasma density with solar illumination affecting radar beam propagation. However, it is found that the irregularity occurrence during the night is higher than expected from ray tracing simulations based on a standard ionospheric density model. The high occurrence at night implies an additional source of plasma density and it is proposed that large-scale density enhancements called polar patches may be the source of this density. Additionally, occurrence maximizes around the terminator due to different competing irregularity production processes that favor a more or less sunlit ionosphere. The second study is concerned with modeling irregularity characterics near a largescale density gradient reversal, such as those expected near polar patches, with a particular ...
author2 Makarevich, Roman
Bristow, William
Conde, Mark
Zhang, Hui
format Doctoral or Postdoctoral Thesis
author Lamarche, Leslie
spellingShingle Lamarche, Leslie
Plasma irregularity production in the polar cap f-region ionosphere
author_facet Lamarche, Leslie
author_sort Lamarche, Leslie
title Plasma irregularity production in the polar cap f-region ionosphere
title_short Plasma irregularity production in the polar cap f-region ionosphere
title_full Plasma irregularity production in the polar cap f-region ionosphere
title_fullStr Plasma irregularity production in the polar cap f-region ionosphere
title_full_unstemmed Plasma irregularity production in the polar cap f-region ionosphere
title_sort plasma irregularity production in the polar cap f-region ionosphere
publishDate 2017
url http://hdl.handle.net/11122/7619
geographic Fairbanks
geographic_facet Fairbanks
genre Antarc*
Antarctica
Alaska
genre_facet Antarc*
Antarctica
Alaska
op_relation http://hdl.handle.net/11122/7619
Department of Physics
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