Assimilation of virtual wide swath altimetry to improve Arctic river modeling

International audience Global surface water variations are still difficult to monitor with current satellite measurements. The future Surface Water and Ocean Topography (SWOT) mission is designed to address this issue. Its main payload will be a wide swath altimeter which will provide maps of water...

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Published in:Remote Sensing of Environment
Main Authors: Biancamaria, Sylvain, Durand, Michael, Andreadis, Kostantinos, Bates, Paul, Boone, Aaron, Mognard, Nelly, Rodriguez, Ernesto, Alsdorf, Doug, Lettenmaier, D. P., Clark, Elizabeth
Other Authors: Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Byrd Polar Research Center, Ohio State University Columbus (OSU), School of Geographical Sciences Bristol, University of Bristol Bristol, Groupe d'étude de l'atmosphère météorologique (CNRM-GAME), Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), School of Earth Sciences, Department of Civil and Environmental Engineering, University of Washington, University of Washington Seattle, CNES TOSCA SWOT; NASA's programs in Physical Oceanography and Terrestrial Hydrology; OSU Climate, Water, and Carbon Program; CNES/Noveltis grant., European Project:
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
geo
Online Access:https://doi.org/10.1016/j.rse.2010.09.008
https://hal.archives-ouvertes.fr/hal-00575528/file/Biancamaria_etal_2011_RSE.pdf
https://hal.archives-ouvertes.fr/hal-00575528
id fttriple:oai:gotriple.eu:10670/1.hnp6p5
record_format openpolar
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic SWOT
Wide swath altimetry
Hydrologic/hydraulic modeling
Data assimilation
Kalman filter
Kalman smoother
Arctic
Ob River
envir
geo
spellingShingle SWOT
Wide swath altimetry
Hydrologic/hydraulic modeling
Data assimilation
Kalman filter
Kalman smoother
Arctic
Ob River
envir
geo
Biancamaria, Sylvain
Durand, Michael
Andreadis, Kostantinos,
Bates, Paul
Boone, Aaron
Mognard, Nelly
Rodriguez, Ernesto
Alsdorf, Doug
Lettenmaier, D. P.
Clark, Elizabeth
Assimilation of virtual wide swath altimetry to improve Arctic river modeling
topic_facet SWOT
Wide swath altimetry
Hydrologic/hydraulic modeling
Data assimilation
Kalman filter
Kalman smoother
Arctic
Ob River
envir
geo
description International audience Global surface water variations are still difficult to monitor with current satellite measurements. The future Surface Water and Ocean Topography (SWOT) mission is designed to address this issue. Its main payload will be a wide swath altimeter which will provide maps of water surface elevations between 78°S and 78°N over a 120 km swath. This study aims to combine coupled hydrologic/hydraulic modeling of an Arctic river with virtual SWOT observations using a local ensemble Kalman smoother to characterize river water depth variations. We assumed that modeling errors are only due to uncertainties in atmospheric forcing fields (precipitation and air temperature) and different SWOT orbits were tested. First, we tested orbits that all have a three day repeat period but differ in terms of their spatial coverage of the study reach; these orbits correspond to the first three months of the mission, which will be dedicated to calibration and validation experiments. For these orbits, the mean spatial Root Mean Square Error (RMSE) in modeled channel water depth decreased by between 29 % and 79 % compared to the modeled RMSE with no assimilation, depending on the spatial coverage. The corresponding mean temporal RMSE decrease was between 54 % and 91 %. We then tested the nominal orbit with a twenty two day repeat period which will be used during the remaining lifetime of the mission. Unlike the three day repeat orbits, this orbit will observe all continental surfaces (except Antartica and the northern part of Greenland) during one repeat period. The assimilation of SWOT observations computed with this nominal orbit into the hydraulic model leads to a decrease of 59 % and 66 % in the mean spatial and temporal RMSE in modeled channel water depth, respectively. These results show the huge potential of the future SWOT mission for land surface hydrology, especially at high latitudes which will be very well sampled during one orbit repeat period. Still, further work is needed to reduce current modeling ...
author2 Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)
Byrd Polar Research Center
Ohio State University Columbus (OSU)
School of Geographical Sciences Bristol
University of Bristol Bristol
Groupe d'étude de l'atmosphère météorologique (CNRM-GAME)
Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS)
Jet Propulsion Laboratory (JPL)
NASA-California Institute of Technology (CALTECH)
School of Earth Sciences
Department of Civil and Environmental Engineering, University of Washington
University of Washington Seattle
CNES TOSCA SWOT; NASA's programs in Physical Oceanography and Terrestrial Hydrology; OSU Climate, Water, and Carbon Program; CNES/Noveltis grant.
European Project:
format Article in Journal/Newspaper
author Biancamaria, Sylvain
Durand, Michael
Andreadis, Kostantinos,
Bates, Paul
Boone, Aaron
Mognard, Nelly
Rodriguez, Ernesto
Alsdorf, Doug
Lettenmaier, D. P.
Clark, Elizabeth
author_facet Biancamaria, Sylvain
Durand, Michael
Andreadis, Kostantinos,
Bates, Paul
Boone, Aaron
Mognard, Nelly
Rodriguez, Ernesto
Alsdorf, Doug
Lettenmaier, D. P.
Clark, Elizabeth
author_sort Biancamaria, Sylvain
title Assimilation of virtual wide swath altimetry to improve Arctic river modeling
title_short Assimilation of virtual wide swath altimetry to improve Arctic river modeling
title_full Assimilation of virtual wide swath altimetry to improve Arctic river modeling
title_fullStr Assimilation of virtual wide swath altimetry to improve Arctic river modeling
title_full_unstemmed Assimilation of virtual wide swath altimetry to improve Arctic river modeling
title_sort assimilation of virtual wide swath altimetry to improve arctic river modeling
publisher HAL CCSD
publishDate 2011
url https://doi.org/10.1016/j.rse.2010.09.008
https://hal.archives-ouvertes.fr/hal-00575528/file/Biancamaria_etal_2011_RSE.pdf
https://hal.archives-ouvertes.fr/hal-00575528
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre antartic*
Arctic
Greenland
ob river
genre_facet antartic*
Arctic
Greenland
ob river
op_source Hyper Article en Ligne - Sciences de l'Homme et de la Société
ISSN: 0034-4257
EISSN: 1879-0704
Remote Sensing of Environment
Remote Sensing of Environment, Elsevier, 2011, 115 (2), pp.373-381. ⟨10.1016/j.rse.2010.09.008⟩
op_relation hal-00575528
doi:10.1016/j.rse.2010.09.008
10670/1.hnp6p5
https://hal.archives-ouvertes.fr/hal-00575528/file/Biancamaria_etal_2011_RSE.pdf
https://hal.archives-ouvertes.fr/hal-00575528
op_rights other
op_doi https://doi.org/10.1016/j.rse.2010.09.008
container_title Remote Sensing of Environment
container_volume 115
container_issue 2
container_start_page 373
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spelling fttriple:oai:gotriple.eu:10670/1.hnp6p5 2023-05-15T14:15:32+02:00 Assimilation of virtual wide swath altimetry to improve Arctic river modeling Biancamaria, Sylvain Durand, Michael Andreadis, Kostantinos, Bates, Paul Boone, Aaron Mognard, Nelly Rodriguez, Ernesto Alsdorf, Doug Lettenmaier, D. P. Clark, Elizabeth Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) Byrd Polar Research Center Ohio State University Columbus (OSU) School of Geographical Sciences Bristol University of Bristol Bristol Groupe d'étude de l'atmosphère météorologique (CNRM-GAME) Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS) Jet Propulsion Laboratory (JPL) NASA-California Institute of Technology (CALTECH) School of Earth Sciences Department of Civil and Environmental Engineering, University of Washington University of Washington Seattle CNES TOSCA SWOT; NASA's programs in Physical Oceanography and Terrestrial Hydrology; OSU Climate, Water, and Carbon Program; CNES/Noveltis grant. European Project: 2011-02-01 https://doi.org/10.1016/j.rse.2010.09.008 https://hal.archives-ouvertes.fr/hal-00575528/file/Biancamaria_etal_2011_RSE.pdf https://hal.archives-ouvertes.fr/hal-00575528 en eng HAL CCSD Elsevier hal-00575528 doi:10.1016/j.rse.2010.09.008 10670/1.hnp6p5 https://hal.archives-ouvertes.fr/hal-00575528/file/Biancamaria_etal_2011_RSE.pdf https://hal.archives-ouvertes.fr/hal-00575528 other Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0034-4257 EISSN: 1879-0704 Remote Sensing of Environment Remote Sensing of Environment, Elsevier, 2011, 115 (2), pp.373-381. ⟨10.1016/j.rse.2010.09.008⟩ SWOT Wide swath altimetry Hydrologic/hydraulic modeling Data assimilation Kalman filter Kalman smoother Arctic Ob River envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.1016/j.rse.2010.09.008 2023-01-22T18:24:25Z International audience Global surface water variations are still difficult to monitor with current satellite measurements. The future Surface Water and Ocean Topography (SWOT) mission is designed to address this issue. Its main payload will be a wide swath altimeter which will provide maps of water surface elevations between 78°S and 78°N over a 120 km swath. This study aims to combine coupled hydrologic/hydraulic modeling of an Arctic river with virtual SWOT observations using a local ensemble Kalman smoother to characterize river water depth variations. We assumed that modeling errors are only due to uncertainties in atmospheric forcing fields (precipitation and air temperature) and different SWOT orbits were tested. First, we tested orbits that all have a three day repeat period but differ in terms of their spatial coverage of the study reach; these orbits correspond to the first three months of the mission, which will be dedicated to calibration and validation experiments. For these orbits, the mean spatial Root Mean Square Error (RMSE) in modeled channel water depth decreased by between 29 % and 79 % compared to the modeled RMSE with no assimilation, depending on the spatial coverage. The corresponding mean temporal RMSE decrease was between 54 % and 91 %. We then tested the nominal orbit with a twenty two day repeat period which will be used during the remaining lifetime of the mission. Unlike the three day repeat orbits, this orbit will observe all continental surfaces (except Antartica and the northern part of Greenland) during one repeat period. The assimilation of SWOT observations computed with this nominal orbit into the hydraulic model leads to a decrease of 59 % and 66 % in the mean spatial and temporal RMSE in modeled channel water depth, respectively. These results show the huge potential of the future SWOT mission for land surface hydrology, especially at high latitudes which will be very well sampled during one orbit repeat period. Still, further work is needed to reduce current modeling ... Article in Journal/Newspaper antartic* Arctic Greenland ob river Unknown Arctic Greenland Remote Sensing of Environment 115 2 373 381