Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere

Thesis (M.S.) University of Alaska Fairbanks, 2012 In this thesis a numerical method of calculating ground-scattered power from the results of a ray tracing analysis is presented. The method is based on a conservation of energy approach and offers advantages over an alternative method derived from t...

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Main Author: Theurer, Timothy E.
Format: Thesis
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11122/8421
id ftunivalaska:oai:scholarworks.alaska.edu:11122/8421
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/8421 2023-05-15T17:04:42+02:00 Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere Theurer, Timothy E. 2012-08 http://hdl.handle.net/11122/8421 en_US eng http://hdl.handle.net/11122/8421 Electrical and Computer Engineering Department Ionospheric electron density Super Dual Auroral Radar Network (SuperDARN) Thesis ms 2012 ftunivalaska 2023-02-23T21:37:02Z Thesis (M.S.) University of Alaska Fairbanks, 2012 In this thesis a numerical method of calculating ground-scattered power from the results of a ray tracing analysis is presented. The method is based on a conservation of energy approach and offers advantages over an alternative method derived from the radar equation. The improved numerical method is used to investigate two different physical phenomena by comparison with measured ground-scattered power observed by a high-frequency (HF) radar located in Kodiak, AK that is part of the Super Dual Auroral Radar Network (SuperDARN). First, the effects of artificial electron density layers on observed ground scatter is studied through a comparison of simulated and measured power profiles. The results demonstrate that the location and spatial dimensions of artificial layers may be estimated by a comparison of the location and amplitude of simulated and measured power enhancements. Second, a Monte-Carlo simulation method is used to characterize the temporal distribution of ground-scattered power. Random processes including background electron density perturbations, polarization, noise, and sample correlation are modeled in simulation and used to estimate statistical moment profiles. The simulated statistical moment profiles are compared to measured profiles as a means of model verification and to roughly approximate background electron density perturbations in the ionosphere. Thesis Kodiak Alaska University of Alaska: ScholarWorks@UA Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
topic Ionospheric electron density
Super Dual Auroral Radar Network (SuperDARN)
spellingShingle Ionospheric electron density
Super Dual Auroral Radar Network (SuperDARN)
Theurer, Timothy E.
Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
topic_facet Ionospheric electron density
Super Dual Auroral Radar Network (SuperDARN)
description Thesis (M.S.) University of Alaska Fairbanks, 2012 In this thesis a numerical method of calculating ground-scattered power from the results of a ray tracing analysis is presented. The method is based on a conservation of energy approach and offers advantages over an alternative method derived from the radar equation. The improved numerical method is used to investigate two different physical phenomena by comparison with measured ground-scattered power observed by a high-frequency (HF) radar located in Kodiak, AK that is part of the Super Dual Auroral Radar Network (SuperDARN). First, the effects of artificial electron density layers on observed ground scatter is studied through a comparison of simulated and measured power profiles. The results demonstrate that the location and spatial dimensions of artificial layers may be estimated by a comparison of the location and amplitude of simulated and measured power enhancements. Second, a Monte-Carlo simulation method is used to characterize the temporal distribution of ground-scattered power. Random processes including background electron density perturbations, polarization, noise, and sample correlation are modeled in simulation and used to estimate statistical moment profiles. The simulated statistical moment profiles are compared to measured profiles as a means of model verification and to roughly approximate background electron density perturbations in the ionosphere.
format Thesis
author Theurer, Timothy E.
author_facet Theurer, Timothy E.
author_sort Theurer, Timothy E.
title Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
title_short Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
title_full Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
title_fullStr Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
title_full_unstemmed Ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
title_sort ray tracing applications for high-frequency radar: characterizing artificial layers and background density perturbations in the ionosphere
publishDate 2012
url http://hdl.handle.net/11122/8421
geographic Fairbanks
geographic_facet Fairbanks
genre Kodiak
Alaska
genre_facet Kodiak
Alaska
op_relation http://hdl.handle.net/11122/8421
Electrical and Computer Engineering Department
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