GNSS signal reflections off sea ice

Multipath has a deleterious effect on GNSS positioning applications, but on the other hand is extremely beneficial to reflectometry, a field of science that is of utmost importance nowadays. Using GPS and/or GLONASS signals for low elevation angles, one can take advantage of this effect. Direct and...

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Bibliographic Details
Main Author: Eleftherios Christos, Drosinos
Other Authors: Chalmers tekniska högskola / Institutionen för rymd- och geovetenskap, Chalmers University of Technology / Department of Earth and Space Sciences
Format: Other/Unknown Material
Language:English
Published: 2019
Subjects:
Online Access:https://hdl.handle.net/20.500.12380/246359
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spelling ftchalmersuniojs:oai:odr.chalmers.se:20.500.12380/246359 2023-07-30T04:06:46+02:00 GNSS signal reflections off sea ice Eleftherios Christos, Drosinos Chalmers tekniska högskola / Institutionen för rymd- och geovetenskap Chalmers University of Technology / Department of Earth and Space Sciences 2019-07-03T14:24:25Z application/pdf https://hdl.handle.net/20.500.12380/246359 eng eng https://hdl.handle.net/20.500.12380/246359 Grundläggande vetenskaper Klimatforskning Geofysik Signalbehandling Basic Sciences Climate Research Geophysics Signal Processing H 2019 ftchalmersuniojs https://doi.org/20.500.12380/246359 2023-07-08T19:57:25Z Multipath has a deleterious effect on GNSS positioning applications, but on the other hand is extremely beneficial to reflectometry, a field of science that is of utmost importance nowadays. Using GPS and/or GLONASS signals for low elevation angles, one can take advantage of this effect. Direct and reflected GNSS signals interfere with each other to form multipath signals, the composite SNR of which is recorded by a GNSS antenna connected to a receiver. While the satellites move across the sky, an interference pattern can be observed, which for low elevation angles can be very useful and one can calculate the reflector’s height (distance between the antenna phase centre and the reflection surface). In this thesis, the SNR analysis technique was used to isolate the amplitude and the damping factor of dSNR in order to draw conclusions about the sea-surface conditions under freeze states in the vicinity of the GNSS-R station installed in Onsala Space Observatory. It is shown that the damping factor is more sensitive to reflected signals, than the amplitude and thus can indicate whether there is ice or not near a GNSS-R tide gauge. Other/Unknown Material Sea ice Chalmers University of Technology: Chalmers Open Digital Repository (ODR)
institution Open Polar
collection Chalmers University of Technology: Chalmers Open Digital Repository (ODR)
op_collection_id ftchalmersuniojs
language English
topic Grundläggande vetenskaper
Klimatforskning
Geofysik
Signalbehandling
Basic Sciences
Climate Research
Geophysics
Signal Processing
spellingShingle Grundläggande vetenskaper
Klimatforskning
Geofysik
Signalbehandling
Basic Sciences
Climate Research
Geophysics
Signal Processing
Eleftherios Christos, Drosinos
GNSS signal reflections off sea ice
topic_facet Grundläggande vetenskaper
Klimatforskning
Geofysik
Signalbehandling
Basic Sciences
Climate Research
Geophysics
Signal Processing
description Multipath has a deleterious effect on GNSS positioning applications, but on the other hand is extremely beneficial to reflectometry, a field of science that is of utmost importance nowadays. Using GPS and/or GLONASS signals for low elevation angles, one can take advantage of this effect. Direct and reflected GNSS signals interfere with each other to form multipath signals, the composite SNR of which is recorded by a GNSS antenna connected to a receiver. While the satellites move across the sky, an interference pattern can be observed, which for low elevation angles can be very useful and one can calculate the reflector’s height (distance between the antenna phase centre and the reflection surface). In this thesis, the SNR analysis technique was used to isolate the amplitude and the damping factor of dSNR in order to draw conclusions about the sea-surface conditions under freeze states in the vicinity of the GNSS-R station installed in Onsala Space Observatory. It is shown that the damping factor is more sensitive to reflected signals, than the amplitude and thus can indicate whether there is ice or not near a GNSS-R tide gauge.
author2 Chalmers tekniska högskola / Institutionen för rymd- och geovetenskap
Chalmers University of Technology / Department of Earth and Space Sciences
format Other/Unknown Material
author Eleftherios Christos, Drosinos
author_facet Eleftherios Christos, Drosinos
author_sort Eleftherios Christos, Drosinos
title GNSS signal reflections off sea ice
title_short GNSS signal reflections off sea ice
title_full GNSS signal reflections off sea ice
title_fullStr GNSS signal reflections off sea ice
title_full_unstemmed GNSS signal reflections off sea ice
title_sort gnss signal reflections off sea ice
publishDate 2019
url https://hdl.handle.net/20.500.12380/246359
genre Sea ice
genre_facet Sea ice
op_relation https://hdl.handle.net/20.500.12380/246359
op_doi https://doi.org/20.500.12380/246359
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