An updated and quality controlled surface mass balance dataset for Antarctica
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE We present an updated and quality controlled surface mass balance (SMB) database for the Antarctic ice sheet. Importantly, the database includes formatted metadata, such as measurement technique, elevation, time covered, etc, which allows any user to filte...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2013
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Online Access: | https://hal.science/hal-00923553 https://hal.science/hal-00923553/document https://hal.science/hal-00923553/file/gr2013-pub00039484.pdf https://doi.org/10.5194/tc-7-583-2013 |
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ftunigrenoble:oai:HAL:hal-00923553v1 |
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Open Polar |
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Université Grenoble Alpes: HAL |
op_collection_id |
ftunigrenoble |
language |
English |
topic |
BILAN DE MASSE BASE DE DONNEES MESURE ANTARCTIQUE [SDE]Environmental Sciences |
spellingShingle |
BILAN DE MASSE BASE DE DONNEES MESURE ANTARCTIQUE [SDE]Environmental Sciences Favier, V. Agosta, C. Parouty, S. Durand, Geoffroy Delaygue, G. Gallee, H. Drouet, A.S. Trouvilliez, A. Krinner, G. An updated and quality controlled surface mass balance dataset for Antarctica |
topic_facet |
BILAN DE MASSE BASE DE DONNEES MESURE ANTARCTIQUE [SDE]Environmental Sciences |
description |
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE We present an updated and quality controlled surface mass balance (SMB) database for the Antarctic ice sheet. Importantly, the database includes formatted metadata, such as measurement technique, elevation, time covered, etc, which allows any user to filter out the data. Here, we discard data with limited spatial and temporal representativeness, too small measurement accuracy, or lack of quality control. Applied to the database, this filtering process gives four times more reliable data than when applied to previously available databases. New data with high spatial resolution are now available over long traverses, and at low elevation in some areas. However, the quality control led to a considerable reduction in the spatial density of data in several regions, particularly over West Antarctica. Over interior plateaus, where the SMB is low, the spatial density of measurements remains high. This quality controlled dataset was compared to results from ERA-Interim reanalysis to assess whether field data allow us to reconstruct an accurate description of the main SMB distribution features in Antarctica. We identified large areas where data gaps impede model validation: except for very few areas (e. g., Adelie Land), measurements in the elevation range between 200 m and 1000 m above sea level are not regularly distributed and do not allow a thorough validation of models in such regions with complex topography, where the highest scattering of SMB values is reported. Clearly, increasing the spatial density of field measurements at low elevations, in the Antarctic Peninsula and in West Antarctica is a scientific priority. |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) |
format |
Article in Journal/Newspaper |
author |
Favier, V. Agosta, C. Parouty, S. Durand, Geoffroy Delaygue, G. Gallee, H. Drouet, A.S. Trouvilliez, A. Krinner, G. |
author_facet |
Favier, V. Agosta, C. Parouty, S. Durand, Geoffroy Delaygue, G. Gallee, H. Drouet, A.S. Trouvilliez, A. Krinner, G. |
author_sort |
Favier, V. |
title |
An updated and quality controlled surface mass balance dataset for Antarctica |
title_short |
An updated and quality controlled surface mass balance dataset for Antarctica |
title_full |
An updated and quality controlled surface mass balance dataset for Antarctica |
title_fullStr |
An updated and quality controlled surface mass balance dataset for Antarctica |
title_full_unstemmed |
An updated and quality controlled surface mass balance dataset for Antarctica |
title_sort |
updated and quality controlled surface mass balance dataset for antarctica |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00923553 https://hal.science/hal-00923553/document https://hal.science/hal-00923553/file/gr2013-pub00039484.pdf https://doi.org/10.5194/tc-7-583-2013 |
geographic |
Antarctic Antarctic Peninsula The Antarctic West Antarctica |
geographic_facet |
Antarctic Antarctic Peninsula The Antarctic West Antarctica |
genre |
Adelie Land Antarc* Antarctic Antarctic Peninsula Antarctica Antarctique* Ice Sheet The Cryosphere West Antarctica |
genre_facet |
Adelie Land Antarc* Antarctic Antarctic Peninsula Antarctica Antarctique* Ice Sheet The Cryosphere West Antarctica |
op_source |
ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.science/hal-00923553 The Cryosphere, 2013, 7 (2), p. 583 - p. 597. ⟨10.5194/tc-7-583-2013⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-7-583-2013 hal-00923553 https://hal.science/hal-00923553 https://hal.science/hal-00923553/document https://hal.science/hal-00923553/file/gr2013-pub00039484.pdf doi:10.5194/tc-7-583-2013 IRSTEA: PUB00039484 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/tc-7-583-2013 |
container_title |
The Cryosphere |
container_volume |
7 |
container_issue |
2 |
container_start_page |
583 |
op_container_end_page |
597 |
_version_ |
1796318004029423616 |
spelling |
ftunigrenoble:oai:HAL:hal-00923553v1 2024-04-14T08:00:14+00:00 An updated and quality controlled surface mass balance dataset for Antarctica Favier, V. Agosta, C. Parouty, S. Durand, Geoffroy Delaygue, G. Gallee, H. Drouet, A.S. Trouvilliez, A. Krinner, G. Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) 2013 https://hal.science/hal-00923553 https://hal.science/hal-00923553/document https://hal.science/hal-00923553/file/gr2013-pub00039484.pdf https://doi.org/10.5194/tc-7-583-2013 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-7-583-2013 hal-00923553 https://hal.science/hal-00923553 https://hal.science/hal-00923553/document https://hal.science/hal-00923553/file/gr2013-pub00039484.pdf doi:10.5194/tc-7-583-2013 IRSTEA: PUB00039484 info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.science/hal-00923553 The Cryosphere, 2013, 7 (2), p. 583 - p. 597. ⟨10.5194/tc-7-583-2013⟩ BILAN DE MASSE BASE DE DONNEES MESURE ANTARCTIQUE [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2013 ftunigrenoble https://doi.org/10.5194/tc-7-583-2013 2024-03-21T16:04:18Z [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE We present an updated and quality controlled surface mass balance (SMB) database for the Antarctic ice sheet. Importantly, the database includes formatted metadata, such as measurement technique, elevation, time covered, etc, which allows any user to filter out the data. Here, we discard data with limited spatial and temporal representativeness, too small measurement accuracy, or lack of quality control. Applied to the database, this filtering process gives four times more reliable data than when applied to previously available databases. New data with high spatial resolution are now available over long traverses, and at low elevation in some areas. However, the quality control led to a considerable reduction in the spatial density of data in several regions, particularly over West Antarctica. Over interior plateaus, where the SMB is low, the spatial density of measurements remains high. This quality controlled dataset was compared to results from ERA-Interim reanalysis to assess whether field data allow us to reconstruct an accurate description of the main SMB distribution features in Antarctica. We identified large areas where data gaps impede model validation: except for very few areas (e. g., Adelie Land), measurements in the elevation range between 200 m and 1000 m above sea level are not regularly distributed and do not allow a thorough validation of models in such regions with complex topography, where the highest scattering of SMB values is reported. Clearly, increasing the spatial density of field measurements at low elevations, in the Antarctic Peninsula and in West Antarctica is a scientific priority. Article in Journal/Newspaper Adelie Land Antarc* Antarctic Antarctic Peninsula Antarctica Antarctique* Ice Sheet The Cryosphere West Antarctica Université Grenoble Alpes: HAL Antarctic Antarctic Peninsula The Antarctic West Antarctica The Cryosphere 7 2 583 597 |