The Ice-Free Topography of Svalbard

International audience We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving approach for mapping glacier ice thickness. SVIFT1.0 is informed by more than 1 million point measurements, totalling more than 8,700 km of thickness profiles. SVIFT1.0 is publicly...

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Published in:Geophysical Research Letters
Main Authors: Fürst, Johannes, Navarro, Francisco, Gillet-Chaulet, Fabien, Huss, Matthias, Moholdt, Geir, Fettweis, Xavier, Lang, Charlotte, Seehaus, Thorsten, Ai, Songtao, Benham, Toby, Benn, Douglas, Björnsson, Helgi, Dowdeswell, Julian, Grabiec, Mariusz, Kohler, Jack, Lavrentiev, Ivan, Lindbäck, Katrin, Melvold, Kjetil, Pettersson, Rickard, Rippin, David, Saintenoy, Albane, Sánchez-Gámez, Pablo, Schüler, Thomas, Sevestre, Heïdi, Vasilenko, Evgeny, Braun, Matthias
Other Authors: Friedrich-Alexander Universität Erlangen-Nürnberg = University of Erlangen-Nuremberg (FAU), University Politecnica de Madrid, Centre for Automation and Robotics (UPM - CSIC), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université de Fribourg = University of Fribourg (UNIFR), Laboratory of Hydraulics, Hydrology and Glaciology, Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), Norwegian Polar Institute, Université de Liège, Wuhan University China, University of Cambridge UK (CAM), University of Saint Andrews, University of Iceland Reykjavik, University of Silesia in Katowice, Institute of Geography of RAS, Russian Academy of Sciences Moscow (RAS), Norwegian Water Resources and Energy Directorate (NVE), Uppsala University, University of York York, UK, Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Universidad Politécnica de Madrid (UPM), University of Oslo (UiO), The University Centre in Svalbard (UNIS), Uzbekistan Academy of Sciences
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2018
Subjects:
Online Access:https://hal.science/hal-01967441
https://hal.science/hal-01967441/document
https://hal.science/hal-01967441/file/2018GL079734.pdf
https://doi.org/10.1029/2018GL079734
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spelling ftuniparissaclay:oai:HAL:hal-01967441v1 2024-06-16T07:40:12+00:00 The Ice-Free Topography of Svalbard Fürst, Johannes Navarro, Francisco Gillet-Chaulet, Fabien Huss, Matthias Moholdt, Geir Fettweis, Xavier Lang, Charlotte Seehaus, Thorsten Ai, Songtao Benham, Toby Benn, Douglas Björnsson, Helgi Dowdeswell, Julian Grabiec, Mariusz Kohler, Jack Lavrentiev, Ivan Lindbäck, Katrin Melvold, Kjetil Pettersson, Rickard Rippin, David Saintenoy, Albane Sánchez-Gámez, Pablo Schüler, Thomas Sevestre, Heïdi Vasilenko, Evgeny Braun, Matthias Friedrich-Alexander Universität Erlangen-Nürnberg = University of Erlangen-Nuremberg (FAU) University Politecnica de Madrid, Centre for Automation and Robotics (UPM - CSIC) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université de Fribourg = University of Fribourg (UNIFR) Laboratory of Hydraulics, Hydrology and Glaciology Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Norwegian Polar Institute Université de Liège Wuhan University China University of Cambridge UK (CAM) University of Saint Andrews University of Iceland Reykjavik University of Silesia in Katowice Institute of Geography of RAS Russian Academy of Sciences Moscow (RAS) Norwegian Water Resources and Energy Directorate (NVE) Uppsala University University of York York, UK Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Universidad Politécnica de Madrid (UPM) University of Oslo (UiO) The University Centre in Svalbard (UNIS) Uzbekistan Academy of Sciences 2018-11-16 https://hal.science/hal-01967441 https://hal.science/hal-01967441/document https://hal.science/hal-01967441/file/2018GL079734.pdf https://doi.org/10.1029/2018GL079734 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2018GL079734 hal-01967441 https://hal.science/hal-01967441 https://hal.science/hal-01967441/document https://hal.science/hal-01967441/file/2018GL079734.pdf doi:10.1029/2018GL079734 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-01967441 Geophysical Research Letters, 2018, 45 (21), pp.11,760-11,769. ⟨10.1029/2018GL079734⟩ [SDU]Sciences of the Universe [physics] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2018 ftuniparissaclay https://doi.org/10.1029/2018GL079734 2024-05-17T00:04:24Z International audience We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving approach for mapping glacier ice thickness. SVIFT1.0 is informed by more than 1 million point measurements, totalling more than 8,700 km of thickness profiles. SVIFT1.0 is publicly available and represents the geometric state around the year 2010. Our estimate for the total ice volume is 6,199 km 3 ,equivalent to 1.5-cm sea level rise. The thickness map suggests that 13% of the glacierized area is grounded below sea level. A complementary map of error estimates comprises uncertainties in the thickness surveys as well as in other input variables. Aggregated error estimates are used to define a likely ice-volume range of 5,200–7,300 km 3. The ice front thickness of marine-terminating glaciers is a key quantity for ice loss attribution because it controls the potential ice discharge by iceberg calving into the ocean. We find a mean ice front thickness of 135 m for the archipelago (likely range 123–158 m) Article in Journal/Newspaper glacier Svalbard Archives ouvertes de Paris-Saclay Svalbard Geophysical Research Letters 45 21
institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic [SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle [SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Fürst, Johannes
Navarro, Francisco
Gillet-Chaulet, Fabien
Huss, Matthias
Moholdt, Geir
Fettweis, Xavier
Lang, Charlotte
Seehaus, Thorsten
Ai, Songtao
Benham, Toby
Benn, Douglas
Björnsson, Helgi
Dowdeswell, Julian
Grabiec, Mariusz
Kohler, Jack
Lavrentiev, Ivan
Lindbäck, Katrin
Melvold, Kjetil
Pettersson, Rickard
Rippin, David
Saintenoy, Albane
Sánchez-Gámez, Pablo
Schüler, Thomas
Sevestre, Heïdi
Vasilenko, Evgeny
Braun, Matthias
The Ice-Free Topography of Svalbard
topic_facet [SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving approach for mapping glacier ice thickness. SVIFT1.0 is informed by more than 1 million point measurements, totalling more than 8,700 km of thickness profiles. SVIFT1.0 is publicly available and represents the geometric state around the year 2010. Our estimate for the total ice volume is 6,199 km 3 ,equivalent to 1.5-cm sea level rise. The thickness map suggests that 13% of the glacierized area is grounded below sea level. A complementary map of error estimates comprises uncertainties in the thickness surveys as well as in other input variables. Aggregated error estimates are used to define a likely ice-volume range of 5,200–7,300 km 3. The ice front thickness of marine-terminating glaciers is a key quantity for ice loss attribution because it controls the potential ice discharge by iceberg calving into the ocean. We find a mean ice front thickness of 135 m for the archipelago (likely range 123–158 m)
author2 Friedrich-Alexander Universität Erlangen-Nürnberg = University of Erlangen-Nuremberg (FAU)
University Politecnica de Madrid, Centre for Automation and Robotics (UPM - CSIC)
Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université de Fribourg = University of Fribourg (UNIFR)
Laboratory of Hydraulics, Hydrology and Glaciology
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)
Norwegian Polar Institute
Université de Liège
Wuhan University China
University of Cambridge UK (CAM)
University of Saint Andrews
University of Iceland Reykjavik
University of Silesia in Katowice
Institute of Geography of RAS
Russian Academy of Sciences Moscow (RAS)
Norwegian Water Resources and Energy Directorate (NVE)
Uppsala University
University of York York, UK
Géosciences Paris Sud (GEOPS)
Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS)
Universidad Politécnica de Madrid (UPM)
University of Oslo (UiO)
The University Centre in Svalbard (UNIS)
Uzbekistan Academy of Sciences
format Article in Journal/Newspaper
author Fürst, Johannes
Navarro, Francisco
Gillet-Chaulet, Fabien
Huss, Matthias
Moholdt, Geir
Fettweis, Xavier
Lang, Charlotte
Seehaus, Thorsten
Ai, Songtao
Benham, Toby
Benn, Douglas
Björnsson, Helgi
Dowdeswell, Julian
Grabiec, Mariusz
Kohler, Jack
Lavrentiev, Ivan
Lindbäck, Katrin
Melvold, Kjetil
Pettersson, Rickard
Rippin, David
Saintenoy, Albane
Sánchez-Gámez, Pablo
Schüler, Thomas
Sevestre, Heïdi
Vasilenko, Evgeny
Braun, Matthias
author_facet Fürst, Johannes
Navarro, Francisco
Gillet-Chaulet, Fabien
Huss, Matthias
Moholdt, Geir
Fettweis, Xavier
Lang, Charlotte
Seehaus, Thorsten
Ai, Songtao
Benham, Toby
Benn, Douglas
Björnsson, Helgi
Dowdeswell, Julian
Grabiec, Mariusz
Kohler, Jack
Lavrentiev, Ivan
Lindbäck, Katrin
Melvold, Kjetil
Pettersson, Rickard
Rippin, David
Saintenoy, Albane
Sánchez-Gámez, Pablo
Schüler, Thomas
Sevestre, Heïdi
Vasilenko, Evgeny
Braun, Matthias
author_sort Fürst, Johannes
title The Ice-Free Topography of Svalbard
title_short The Ice-Free Topography of Svalbard
title_full The Ice-Free Topography of Svalbard
title_fullStr The Ice-Free Topography of Svalbard
title_full_unstemmed The Ice-Free Topography of Svalbard
title_sort ice-free topography of svalbard
publisher HAL CCSD
publishDate 2018
url https://hal.science/hal-01967441
https://hal.science/hal-01967441/document
https://hal.science/hal-01967441/file/2018GL079734.pdf
https://doi.org/10.1029/2018GL079734
geographic Svalbard
geographic_facet Svalbard
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.science/hal-01967441
Geophysical Research Letters, 2018, 45 (21), pp.11,760-11,769. ⟨10.1029/2018GL079734⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2018GL079734
hal-01967441
https://hal.science/hal-01967441
https://hal.science/hal-01967441/document
https://hal.science/hal-01967441/file/2018GL079734.pdf
doi:10.1029/2018GL079734
op_rights http://hal.archives-ouvertes.fr/licences/copyright/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2018GL079734
container_title Geophysical Research Letters
container_volume 45
container_issue 21
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