Monitoring snow water equivalent using the phase of RFID signals
The amount of water contained in a snowpack, known as snow water equivalent (SWE), is used to anticipate the amount of snowmelt that could supply hydroelectric power plants, fill water reservoirs, or sometimes cause flooding. This work introduces a wireless, non-destructive method for monitoring the...
Published in: | The Cryosphere |
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Copernicus Publications
2023
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00067998 2023-08-27T04:12:20+02:00 Monitoring snow water equivalent using the phase of RFID signals Le Breton, Mathieu Larose, Éric Baillet, Laurent Lejeune, Yves van Herwijnen, Alec 2023-08 electronic https://doi.org/10.5194/tc-17-3137-2023 https://noa.gwlb.de/receive/cop_mods_00067998 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00066435/tc-17-3137-2023.pdf https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-17-3137-2023 https://noa.gwlb.de/receive/cop_mods_00067998 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00066435/tc-17-3137-2023.pdf https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2023 ftnonlinearchiv https://doi.org/10.5194/tc-17-3137-2023 2023-08-06T23:19:55Z The amount of water contained in a snowpack, known as snow water equivalent (SWE), is used to anticipate the amount of snowmelt that could supply hydroelectric power plants, fill water reservoirs, or sometimes cause flooding. This work introduces a wireless, non-destructive method for monitoring the SWE of a dry snowpack. The system is based on an array of low-cost passive radiofrequency identification (RFID) tags, placed under the snow and read at 865–868 MHz by a reader located above the snow. The SWE was deduced from the phase delay of the tag's backscattered response, which increases with the amount of snow traversed by the radiofrequency wave. Measurements taken in the laboratory, during snowfall events and over 4.5 months at the Col de Porte test field, were consistent with reference measurements of cosmic rays, precipitation and snow pits. SWE accuracy was ±18 kg m−2 throughout the season (averaged over three tags) and ±3 kg m−2 during dry snowfall events (averaged over data from two antennas and four or five tags). The overall uncertainty compared to snow weighing was ±10 % for snow density in the range 61–390 kg m−3. The main limitations observed were measurement bias caused by wet snow (biased data were discarded) and the need for phase unwrapping. The method has a number of advantages: it allows for continuous measurement (1 min sampling rate in dry snow), it can provide complementary measurement of tag temperature, it does not require the reception of external data, and it opens the way towards spatialized measurements. The results presented also demonstrate that RFID propagation-based sensing can remotely monitor the permittivity of a low-loss dielectric material with scientific-level accuracy. Article in Journal/Newspaper The Cryosphere Niedersächsisches Online-Archiv NOA The Cryosphere 17 8 3137 3156 |
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Niedersächsisches Online-Archiv NOA |
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article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Le Breton, Mathieu Larose, Éric Baillet, Laurent Lejeune, Yves van Herwijnen, Alec Monitoring snow water equivalent using the phase of RFID signals |
topic_facet |
article Verlagsveröffentlichung |
description |
The amount of water contained in a snowpack, known as snow water equivalent (SWE), is used to anticipate the amount of snowmelt that could supply hydroelectric power plants, fill water reservoirs, or sometimes cause flooding. This work introduces a wireless, non-destructive method for monitoring the SWE of a dry snowpack. The system is based on an array of low-cost passive radiofrequency identification (RFID) tags, placed under the snow and read at 865–868 MHz by a reader located above the snow. The SWE was deduced from the phase delay of the tag's backscattered response, which increases with the amount of snow traversed by the radiofrequency wave. Measurements taken in the laboratory, during snowfall events and over 4.5 months at the Col de Porte test field, were consistent with reference measurements of cosmic rays, precipitation and snow pits. SWE accuracy was ±18 kg m−2 throughout the season (averaged over three tags) and ±3 kg m−2 during dry snowfall events (averaged over data from two antennas and four or five tags). The overall uncertainty compared to snow weighing was ±10 % for snow density in the range 61–390 kg m−3. The main limitations observed were measurement bias caused by wet snow (biased data were discarded) and the need for phase unwrapping. The method has a number of advantages: it allows for continuous measurement (1 min sampling rate in dry snow), it can provide complementary measurement of tag temperature, it does not require the reception of external data, and it opens the way towards spatialized measurements. The results presented also demonstrate that RFID propagation-based sensing can remotely monitor the permittivity of a low-loss dielectric material with scientific-level accuracy. |
format |
Article in Journal/Newspaper |
author |
Le Breton, Mathieu Larose, Éric Baillet, Laurent Lejeune, Yves van Herwijnen, Alec |
author_facet |
Le Breton, Mathieu Larose, Éric Baillet, Laurent Lejeune, Yves van Herwijnen, Alec |
author_sort |
Le Breton, Mathieu |
title |
Monitoring snow water equivalent using the phase of RFID signals |
title_short |
Monitoring snow water equivalent using the phase of RFID signals |
title_full |
Monitoring snow water equivalent using the phase of RFID signals |
title_fullStr |
Monitoring snow water equivalent using the phase of RFID signals |
title_full_unstemmed |
Monitoring snow water equivalent using the phase of RFID signals |
title_sort |
monitoring snow water equivalent using the phase of rfid signals |
publisher |
Copernicus Publications |
publishDate |
2023 |
url |
https://doi.org/10.5194/tc-17-3137-2023 https://noa.gwlb.de/receive/cop_mods_00067998 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00066435/tc-17-3137-2023.pdf https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_relation |
The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-17-3137-2023 https://noa.gwlb.de/receive/cop_mods_00067998 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00066435/tc-17-3137-2023.pdf https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-17-3137-2023 |
container_title |
The Cryosphere |
container_volume |
17 |
container_issue |
8 |
container_start_page |
3137 |
op_container_end_page |
3156 |
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1775356366414675968 |