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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: M. Le Breton, É. Larose, L. Baillet, Y. Lejeune, A. van Herwijnen
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-3137-2023
https://doaj.org/article/25d42fc5938d4bf5b8c90cbd625ad0e5
id ftdoajarticles:oai:doaj.org/article:25d42fc5938d4bf5b8c90cbd625ad0e5
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:25d42fc5938d4bf5b8c90cbd625ad0e5 2023-08-27T04:12:20+02:00 Monitoring snow water equivalent using the phase of RFID signals M. Le Breton É. Larose L. Baillet Y. Lejeune A. van Herwijnen 2023-08-01T00:00:00Z https://doi.org/10.5194/tc-17-3137-2023 https://doaj.org/article/25d42fc5938d4bf5b8c90cbd625ad0e5 EN eng Copernicus Publications https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-17-3137-2023 1994-0416 1994-0424 https://doaj.org/article/25d42fc5938d4bf5b8c90cbd625ad0e5 The Cryosphere, Vol 17, Pp 3137-3156 (2023) Environmental sciences GE1-350 Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.5194/tc-17-3137-2023 2023-08-06T00:34:49Z 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 Directory of Open Access Journals: DOAJ Articles The Cryosphere 17 8 3137 3156
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
M. Le Breton
É. Larose
L. Baillet
Y. Lejeune
A. van Herwijnen
Monitoring snow water equivalent using the phase of RFID signals
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
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 M. Le Breton
É. Larose
L. Baillet
Y. Lejeune
A. van Herwijnen
author_facet M. Le Breton
É. Larose
L. Baillet
Y. Lejeune
A. van Herwijnen
author_sort M. Le Breton
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://doaj.org/article/25d42fc5938d4bf5b8c90cbd625ad0e5
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 17, Pp 3137-3156 (2023)
op_relation https://tc.copernicus.org/articles/17/3137/2023/tc-17-3137-2023.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-17-3137-2023
1994-0416
1994-0424
https://doaj.org/article/25d42fc5938d4bf5b8c90cbd625ad0e5
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
_version_ 1775356365873610752