Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014
Remote sensing is a powerful method to reconstruct annual mass-balance series over past decades by exploiting archives of available images, as well as to study glaciers in inaccessible regions. We present the application of a methodological framework based only on optical satellite images to retriev...
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ftdoajarticles:oai:doaj.org/article:24c735dddf8e4d359de60c64704b39f2 2023-05-15T16:57:36+02:00 Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 ANTOINE RABATEL JEAN PIERRE DEDIEU CHRISTIAN VINCENT 2016-12-01T00:00:00Z https://doi.org/10.1017/jog.2016.113 https://doaj.org/article/24c735dddf8e4d359de60c64704b39f2 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143016001131/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.113 0022-1430 1727-5652 https://doaj.org/article/24c735dddf8e4d359de60c64704b39f2 Journal of Glaciology, Vol 62, Pp 1153-1166 (2016) annual surface mass balance mountain glaciers satellite remote sensing snow line Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2016 ftdoajarticles https://doi.org/10.1017/jog.2016.113 2023-03-12T01:30:59Z Remote sensing is a powerful method to reconstruct annual mass-balance series over past decades by exploiting archives of available images, as well as to study glaciers in inaccessible regions. We present the application of a methodological framework based only on optical satellite images to retrieve glacier-wide annual mass balances for 30 glaciers in the French Alps. The glacier-wide annual mass balance for the period 1983–2014 was reconstructed by combining changes in glacier volumes computed from remote-sensing derived DEMs with annual measurements of the snow line altitude on satellite images. Data from direct observations on two of the glaciers confirmed the accuracy of the annual mass balances quantified by remote sensing with an average difference of ~0.3 m w.e., within the uncertainty range of the methods. Our results confirm the significant increase in mass loss since the early 2000s, with a difference >1 m w.e. a−1 between the periods 1983–2002 and 2003–14. The region-wide mass balance for the French Alps over the period 1979–2011 was −0.66 ± 0.27 m w.e. a−1, close to that of the European Alps. We also show that changes in glacier surface area or length are not representative of changes in mass balance at the scale of a few decades. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 62 236 1153 1166 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
annual surface mass balance mountain glaciers satellite remote sensing snow line Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
annual surface mass balance mountain glaciers satellite remote sensing snow line Environmental sciences GE1-350 Meteorology. Climatology QC851-999 ANTOINE RABATEL JEAN PIERRE DEDIEU CHRISTIAN VINCENT Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
topic_facet |
annual surface mass balance mountain glaciers satellite remote sensing snow line Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Remote sensing is a powerful method to reconstruct annual mass-balance series over past decades by exploiting archives of available images, as well as to study glaciers in inaccessible regions. We present the application of a methodological framework based only on optical satellite images to retrieve glacier-wide annual mass balances for 30 glaciers in the French Alps. The glacier-wide annual mass balance for the period 1983–2014 was reconstructed by combining changes in glacier volumes computed from remote-sensing derived DEMs with annual measurements of the snow line altitude on satellite images. Data from direct observations on two of the glaciers confirmed the accuracy of the annual mass balances quantified by remote sensing with an average difference of ~0.3 m w.e., within the uncertainty range of the methods. Our results confirm the significant increase in mass loss since the early 2000s, with a difference >1 m w.e. a−1 between the periods 1983–2002 and 2003–14. The region-wide mass balance for the French Alps over the period 1979–2011 was −0.66 ± 0.27 m w.e. a−1, close to that of the European Alps. We also show that changes in glacier surface area or length are not representative of changes in mass balance at the scale of a few decades. |
format |
Article in Journal/Newspaper |
author |
ANTOINE RABATEL JEAN PIERRE DEDIEU CHRISTIAN VINCENT |
author_facet |
ANTOINE RABATEL JEAN PIERRE DEDIEU CHRISTIAN VINCENT |
author_sort |
ANTOINE RABATEL |
title |
Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
title_short |
Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
title_full |
Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
title_fullStr |
Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
title_full_unstemmed |
Spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the French Alps for the period 1983–2014 |
title_sort |
spatio-temporal changes in glacier-wide mass balance quantified by optical remote sensing on 30 glaciers in the french alps for the period 1983–2014 |
publisher |
Cambridge University Press |
publishDate |
2016 |
url |
https://doi.org/10.1017/jog.2016.113 https://doaj.org/article/24c735dddf8e4d359de60c64704b39f2 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 62, Pp 1153-1166 (2016) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143016001131/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.113 0022-1430 1727-5652 https://doaj.org/article/24c735dddf8e4d359de60c64704b39f2 |
op_doi |
https://doi.org/10.1017/jog.2016.113 |
container_title |
Journal of Glaciology |
container_volume |
62 |
container_issue |
236 |
container_start_page |
1153 |
op_container_end_page |
1166 |
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1766049159962427392 |