River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies

<p>River ice is a key component of the cryosphere. Satellite monitoring of river ice is a rapidly developing area of scientific enquiry, which has wide-ranging implications for climate, environmental and socioeconomic applications. Spaceborne radar altimetry is widely used for monitoring river...

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Main Authors: E. Zakharova, S. Agafonova, C. Duguay, N. Frolova, A. Kouraev
Format: Article
Language:English
Published: Copernicus Publications 2021-12-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/15/5387/2021/tc-15-5387-2021.pdf
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author E. Zakharova
E. Zakharova
S. Agafonova
C. Duguay
C. Duguay
N. Frolova
A. Kouraev
author_facet E. Zakharova
E. Zakharova
S. Agafonova
C. Duguay
C. Duguay
N. Frolova
A. Kouraev
author_sort E. Zakharova
collection DOAJ
description <p>River ice is a key component of the cryosphere. Satellite monitoring of river ice is a rapidly developing area of scientific enquiry, which has wide-ranging implications for climate, environmental and socioeconomic applications. Spaceborne radar altimetry is widely used for monitoring river water regimes; however, its potential for the observation of river ice processes and properties has not been demonstrated yet. Using Ku-band backscatter measurements from the Jason-2 and Jason-3 satellite missions (2008–2019), we demonstrate the potential of radar altimetry for the retrieval of river ice phenology dates and ice thickness for the first time. The altimetric measurements were determined to be sensitive enough to detect the first appearance of ice and the beginning of thermal breakup on the lower Ob River (Western Siberia). The uncertainties in the retrieval of ice event timing were within the 10 d repeat cycle of Jason-2 and Jason-3 in 88 %–90 % of the cases analysed. The uncertainties in the river ice thickness retrievals made via empirical relations between the satellite backscatter measurements and in situ observations, expressed as the root mean square error (RMSE), were of 0.07–0.18 m. A novel application of radar altimetry is the prediction of ice bridge road operations, which is demonstrated herein. We established that the dates of ferry closing and ice road opening and closing in the city of Salekhard can be predicted with an accuracy (expressed as RMSE) of 3–5 d.</p>
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spelling doaj.art-5b944b5ecc8b4f4ba978b373261117252022-12-21T22:43:15ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242021-12-01155387540710.5194/tc-15-5387-2021River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studiesE. Zakharova0E. Zakharova1S. Agafonova2C. Duguay3C. Duguay4N. Frolova5A. Kouraev6Water Problems Institute, Russian Academy of Science, Moscow, RussiaEOLA, Toulouse, FranceDepartment of Land Hydrology, Moscow State University, Moscow, RussiaDepartment of Geography and Environmental Management, University of Waterloo, Waterloo, CanadaH2O Geomatics, Waterloo, CanadaDepartment of Land Hydrology, Moscow State University, Moscow, RussiaLEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France<p>River ice is a key component of the cryosphere. Satellite monitoring of river ice is a rapidly developing area of scientific enquiry, which has wide-ranging implications for climate, environmental and socioeconomic applications. Spaceborne radar altimetry is widely used for monitoring river water regimes; however, its potential for the observation of river ice processes and properties has not been demonstrated yet. Using Ku-band backscatter measurements from the Jason-2 and Jason-3 satellite missions (2008–2019), we demonstrate the potential of radar altimetry for the retrieval of river ice phenology dates and ice thickness for the first time. The altimetric measurements were determined to be sensitive enough to detect the first appearance of ice and the beginning of thermal breakup on the lower Ob River (Western Siberia). The uncertainties in the retrieval of ice event timing were within the 10 d repeat cycle of Jason-2 and Jason-3 in 88 %–90 % of the cases analysed. The uncertainties in the river ice thickness retrievals made via empirical relations between the satellite backscatter measurements and in situ observations, expressed as the root mean square error (RMSE), were of 0.07–0.18 m. A novel application of radar altimetry is the prediction of ice bridge road operations, which is demonstrated herein. We established that the dates of ferry closing and ice road opening and closing in the city of Salekhard can be predicted with an accuracy (expressed as RMSE) of 3–5 d.</p>https://tc.copernicus.org/articles/15/5387/2021/tc-15-5387-2021.pdf
spellingShingle E. Zakharova
E. Zakharova
S. Agafonova
C. Duguay
C. Duguay
N. Frolova
A. Kouraev
River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
The Cryosphere
title River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
title_full River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
title_fullStr River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
title_full_unstemmed River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
title_short River ice phenology and thickness from satellite altimetry: potential for ice bridge road operation and climate studies
title_sort river ice phenology and thickness from satellite altimetry potential for ice bridge road operation and climate studies
url https://tc.copernicus.org/articles/15/5387/2021/tc-15-5387-2021.pdf
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