Multifrequency Scintillation in the Polar Caps

In the ionosphere, plasma density structures with scales sizes ranging from a few centimeters to hundreds of kilometers are capable of modifying the phase and amplitude of a radio signal in a rapid random manner in a process called scintillation. The Coherent Electromagnetic Radio Tomography (CERTO)...

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Main Author: Colby, Tate
Other Authors: 2410791
Format: Text
Language:unknown
Published: Scholarly Commons 2022
Subjects:
Online Access:https://commons.erau.edu/edt/691
https://commons.erau.edu/context/edt/article/1721/viewcontent/ColbyT_Thesis_signed.pdf
id ftembryriddleaun:oai:commons.erau.edu:edt-1721
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spelling ftembryriddleaun:oai:commons.erau.edu:edt-1721 2023-10-01T03:54:14+02:00 Multifrequency Scintillation in the Polar Caps Colby, Tate 2410791 2022-12-08T08:00:00Z application/pdf https://commons.erau.edu/edt/691 https://commons.erau.edu/context/edt/article/1721/viewcontent/ColbyT_Thesis_signed.pdf unknown Scholarly Commons https://commons.erau.edu/edt/691 https://commons.erau.edu/context/edt/article/1721/viewcontent/ColbyT_Thesis_signed.pdf Doctoral Dissertations and Master's Theses Scintillation Polar cap Ionosphere Plasma density CERTO CHAIN RISR Other Astrophysics and Astronomy text 2022 ftembryriddleaun 2023-09-02T19:04:18Z In the ionosphere, plasma density structures with scales sizes ranging from a few centimeters to hundreds of kilometers are capable of modifying the phase and amplitude of a radio signal in a rapid random manner in a process called scintillation. The Coherent Electromagnetic Radio Tomography (CERTO) and the Canadian High Arctic Ionospheric Network (CHAIN) are two different networks of scintillation receivers, each with a station in Resolute Bay, Canada. CERTO measures amplitude and phase signals in VHF and UHF while CHAIN measures amplitude and phase signals in the L-band. Through these measurements we can calculate the scintillation indexes, S_4 and sigma_phi to gain insight into the plasma density structures the scintillation originated from. In this Thesis, the processes of detrending and processing VHF sigma_phi from CERTO data and L-band S_4 & sigma_phi CHAIN data are detailed and the resulting scintillation data are analyzed by comparing the time of events to data from the Resolute Bay Incoherent Scatter Radar (RISR), creating histograms of the total scintillation data acquired, and by examining CERTO sigma_phi data results with respect to elevation angle. This work concludes that detrending scintillation data at frequencies other than L-band is not a trivial process and must be given care in order to produce accurate results. Within this work none of the RISR data contained significant plasma density during any of the satellite conjunctions analyzed. The histograms of total VHF and L-band sigma_phi values show more variation in the average VHF sigma_phi values than in the L-band sigma_phi. A positive correlation between the satellites elevation angle and increase in sigma_phi is identified. Text Arctic Canadian High Arctic Ionospheric Network Resolute Bay Embry-Riddle Aeronautical University: ERAU Scholarly Commons Arctic Canada Resolute Bay ENVELOPE(-94.842,-94.842,74.677,74.677)
institution Open Polar
collection Embry-Riddle Aeronautical University: ERAU Scholarly Commons
op_collection_id ftembryriddleaun
language unknown
topic Scintillation
Polar cap
Ionosphere
Plasma density
CERTO
CHAIN
RISR
Other Astrophysics and Astronomy
spellingShingle Scintillation
Polar cap
Ionosphere
Plasma density
CERTO
CHAIN
RISR
Other Astrophysics and Astronomy
Colby, Tate
Multifrequency Scintillation in the Polar Caps
topic_facet Scintillation
Polar cap
Ionosphere
Plasma density
CERTO
CHAIN
RISR
Other Astrophysics and Astronomy
description In the ionosphere, plasma density structures with scales sizes ranging from a few centimeters to hundreds of kilometers are capable of modifying the phase and amplitude of a radio signal in a rapid random manner in a process called scintillation. The Coherent Electromagnetic Radio Tomography (CERTO) and the Canadian High Arctic Ionospheric Network (CHAIN) are two different networks of scintillation receivers, each with a station in Resolute Bay, Canada. CERTO measures amplitude and phase signals in VHF and UHF while CHAIN measures amplitude and phase signals in the L-band. Through these measurements we can calculate the scintillation indexes, S_4 and sigma_phi to gain insight into the plasma density structures the scintillation originated from. In this Thesis, the processes of detrending and processing VHF sigma_phi from CERTO data and L-band S_4 & sigma_phi CHAIN data are detailed and the resulting scintillation data are analyzed by comparing the time of events to data from the Resolute Bay Incoherent Scatter Radar (RISR), creating histograms of the total scintillation data acquired, and by examining CERTO sigma_phi data results with respect to elevation angle. This work concludes that detrending scintillation data at frequencies other than L-band is not a trivial process and must be given care in order to produce accurate results. Within this work none of the RISR data contained significant plasma density during any of the satellite conjunctions analyzed. The histograms of total VHF and L-band sigma_phi values show more variation in the average VHF sigma_phi values than in the L-band sigma_phi. A positive correlation between the satellites elevation angle and increase in sigma_phi is identified.
author2 2410791
format Text
author Colby, Tate
author_facet Colby, Tate
author_sort Colby, Tate
title Multifrequency Scintillation in the Polar Caps
title_short Multifrequency Scintillation in the Polar Caps
title_full Multifrequency Scintillation in the Polar Caps
title_fullStr Multifrequency Scintillation in the Polar Caps
title_full_unstemmed Multifrequency Scintillation in the Polar Caps
title_sort multifrequency scintillation in the polar caps
publisher Scholarly Commons
publishDate 2022
url https://commons.erau.edu/edt/691
https://commons.erau.edu/context/edt/article/1721/viewcontent/ColbyT_Thesis_signed.pdf
long_lat ENVELOPE(-94.842,-94.842,74.677,74.677)
geographic Arctic
Canada
Resolute Bay
geographic_facet Arctic
Canada
Resolute Bay
genre Arctic
Canadian High Arctic Ionospheric Network
Resolute Bay
genre_facet Arctic
Canadian High Arctic Ionospheric Network
Resolute Bay
op_source Doctoral Dissertations and Master's Theses
op_relation https://commons.erau.edu/edt/691
https://commons.erau.edu/context/edt/article/1721/viewcontent/ColbyT_Thesis_signed.pdf
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