On the accuracy of glacier outlines derived from remote sensing data

International audience Deriving glacier outlines from satellite data has become increasingly popular in the past decade. In particular when glacier outlines are used as a base for change assessment, it is important to know how accurate they are. Calculating the accuracy correctly is challenging, as...

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Published in:Annals of Glaciology
Main Authors: Paul, Frank, Barrand N., E., Berthier, Etienne, Bolch, Tobias, 14 Others, &
Other Authors: Universität Zürich Zürich = University of Zurich (UZH), British Antarctic Survey (BAS), Natural Environment Research Council (NERC), GLACIO LEGOS, Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Instituts für Kartographie Dresden (Institute for Cartography), Technische Universität Dresden = Dresden University of Technology (TU Dresden)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal.science/hal-00846333
https://hal.science/hal-00846333/document
https://hal.science/hal-00846333/file/div-class-title-on-the-accuracy-of-glacier-outlines-derived-from-remote-sensing-data-div.pdf
https://doi.org/10.3189/2013AoG63A296
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record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
spellingShingle [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Paul, Frank
Barrand N., E.
Berthier, Etienne
Bolch, Tobias
14 Others, &
On the accuracy of glacier outlines derived from remote sensing data
topic_facet [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
description International audience Deriving glacier outlines from satellite data has become increasingly popular in the past decade. In particular when glacier outlines are used as a base for change assessment, it is important to know how accurate they are. Calculating the accuracy correctly is challenging, as appropriate reference data (e.g. from higher-resolution sensors) are seldom available. Moreover, after the required manual correction of the raw outlines (e.g. for debris cover), such a comparison would only reveal the accuracy of the analyst rather than of the algorithm applied. Here we compare outlines for clean and debris-covered glaciers, as derived from single and multiple digitizing by different or the same analysts on very high- (1 m) and medium-resolution (30 m) remote-sensing data, against each other and to glacier outlines derived from automated classification of Landsat Thematic Mapper data. Results show a high variability in the interpretation of debris-covered glacier parts, largely independent of the spatial resolution (area differences were up to 30%), and an overall good agreement for clean ice with sufficient contrast to the surrounding terrain (differences 5%). The differences of the automatically derived outlines from a reference value are as small as the standard deviation of the manual digitizations from several analysts. Based on these results, we conclude that automated mapping of clean ice is preferable to manual digitization and recommend using the latter method only for required corrections of incorrectly mapped glacier parts (e.g. debris cover, shadow).
author2 Universität Zürich Zürich = University of Zurich (UZH)
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
GLACIO LEGOS
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Instituts für Kartographie Dresden (Institute for Cartography)
Technische Universität Dresden = Dresden University of Technology (TU Dresden)
format Article in Journal/Newspaper
author Paul, Frank
Barrand N., E.
Berthier, Etienne
Bolch, Tobias
14 Others, &
author_facet Paul, Frank
Barrand N., E.
Berthier, Etienne
Bolch, Tobias
14 Others, &
author_sort Paul, Frank
title On the accuracy of glacier outlines derived from remote sensing data
title_short On the accuracy of glacier outlines derived from remote sensing data
title_full On the accuracy of glacier outlines derived from remote sensing data
title_fullStr On the accuracy of glacier outlines derived from remote sensing data
title_full_unstemmed On the accuracy of glacier outlines derived from remote sensing data
title_sort on the accuracy of glacier outlines derived from remote sensing data
publisher HAL CCSD
publishDate 2013
url https://hal.science/hal-00846333
https://hal.science/hal-00846333/document
https://hal.science/hal-00846333/file/div-class-title-on-the-accuracy-of-glacier-outlines-derived-from-remote-sensing-data-div.pdf
https://doi.org/10.3189/2013AoG63A296
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source ISSN: 0260-3055
EISSN: 1727-5644
Annals of Glaciology
https://hal.science/hal-00846333
Annals of Glaciology, 2013, 54 (63), pp.171-182. ⟨10.3189/2013AoG63A296⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3189/2013AoG63A296
hal-00846333
https://hal.science/hal-00846333
https://hal.science/hal-00846333/document
https://hal.science/hal-00846333/file/div-class-title-on-the-accuracy-of-glacier-outlines-derived-from-remote-sensing-data-div.pdf
doi:10.3189/2013AoG63A296
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3189/2013AoG63A296
container_title Annals of Glaciology
container_volume 54
container_issue 63
container_start_page 171
op_container_end_page 182
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spelling ftinsu:oai:HAL:hal-00846333v1 2023-12-17T10:18:41+01:00 On the accuracy of glacier outlines derived from remote sensing data Paul, Frank Barrand N., E. Berthier, Etienne Bolch, Tobias 14 Others, & Universität Zürich Zürich = University of Zurich (UZH) British Antarctic Survey (BAS) Natural Environment Research Council (NERC) GLACIO LEGOS Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Instituts für Kartographie Dresden (Institute for Cartography) Technische Universität Dresden = Dresden University of Technology (TU Dresden) 2013 https://hal.science/hal-00846333 https://hal.science/hal-00846333/document https://hal.science/hal-00846333/file/div-class-title-on-the-accuracy-of-glacier-outlines-derived-from-remote-sensing-data-div.pdf https://doi.org/10.3189/2013AoG63A296 en eng HAL CCSD Cambridge University Press info:eu-repo/semantics/altIdentifier/doi/10.3189/2013AoG63A296 hal-00846333 https://hal.science/hal-00846333 https://hal.science/hal-00846333/document https://hal.science/hal-00846333/file/div-class-title-on-the-accuracy-of-glacier-outlines-derived-from-remote-sensing-data-div.pdf doi:10.3189/2013AoG63A296 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0260-3055 EISSN: 1727-5644 Annals of Glaciology https://hal.science/hal-00846333 Annals of Glaciology, 2013, 54 (63), pp.171-182. ⟨10.3189/2013AoG63A296⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2013 ftinsu https://doi.org/10.3189/2013AoG63A296 2023-11-22T17:36:48Z International audience Deriving glacier outlines from satellite data has become increasingly popular in the past decade. In particular when glacier outlines are used as a base for change assessment, it is important to know how accurate they are. Calculating the accuracy correctly is challenging, as appropriate reference data (e.g. from higher-resolution sensors) are seldom available. Moreover, after the required manual correction of the raw outlines (e.g. for debris cover), such a comparison would only reveal the accuracy of the analyst rather than of the algorithm applied. Here we compare outlines for clean and debris-covered glaciers, as derived from single and multiple digitizing by different or the same analysts on very high- (1 m) and medium-resolution (30 m) remote-sensing data, against each other and to glacier outlines derived from automated classification of Landsat Thematic Mapper data. Results show a high variability in the interpretation of debris-covered glacier parts, largely independent of the spatial resolution (area differences were up to 30%), and an overall good agreement for clean ice with sufficient contrast to the surrounding terrain (differences 5%). The differences of the automatically derived outlines from a reference value are as small as the standard deviation of the manual digitizations from several analysts. Based on these results, we conclude that automated mapping of clean ice is preferable to manual digitization and recommend using the latter method only for required corrections of incorrectly mapped glacier parts (e.g. debris cover, shadow). Article in Journal/Newspaper Annals of Glaciology Institut national des sciences de l'Univers: HAL-INSU Annals of Glaciology 54 63 171 182