Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery
We present geodetic mass-balance estimates for ten glaciers (22.6 ± 1.1 km2) around Volcán Domuyo between 1962 and 2020 (and 46 glaciers covering 29 ± 1.5 km2 between 1984 and 2020), derived from airborne, ASTER and Pléiades imagery. Overall, we find a slightly negative mass balance (−0.15 ± 0.09 m...
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Cambridge University Press
2023
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ftdoajarticles:oai:doaj.org/article:7738ba1181564f04b027fb606aec69e6 2023-05-15T16:57:33+02:00 Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery Daniel Falaschi Etienne Berthier Joaquín M. C. Belart Claudio Bravo Mariano Castro Marcelo Durand Ricardo Villalba 2023-02-01T00:00:00Z https://doi.org/10.1017/jog.2022.43 https://doaj.org/article/7738ba1181564f04b027fb606aec69e6 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000430/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.43 0022-1430 1727-5652 https://doaj.org/article/7738ba1181564f04b027fb606aec69e6 Journal of Glaciology, Vol 69, Pp 40-56 (2023) Glacier mass balance glacier modelling glacier volume mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.43 2023-03-12T01:30:54Z We present geodetic mass-balance estimates for ten glaciers (22.6 ± 1.1 km2) around Volcán Domuyo between 1962 and 2020 (and 46 glaciers covering 29 ± 1.5 km2 between 1984 and 2020), derived from airborne, ASTER and Pléiades imagery. Overall, we find a slightly negative mass balance (−0.15 ± 0.09 m w.e. a–1) for the entire 1962–2020 time span. A closer inspection of sub-periods reveals, however, an increasingly negative mass balance with time. The Domuyo glaciers shifted from a moderately positive mass balance of +0.28 ± 0.13 m w.e. a–1 between 1962 and 1984, to a strongly negative mass balance of −0.99 ± 0.19 m w.e. a–1 between 2012 and 2020. An increase in summer temperatures and a decrease in winter precipitation during the last four decades are likely drivers of the observed glacier changes. We support this finding by implementing a minimal glacier model, relying solely on monthly precipitation and air temperatures. The mass-balance evolution detected in Volcán Domuyo is consistent with other sites spread across the Central Andes, suggesting rapidly increasing glacier wastage impacts are occurring at a geographically wider scale. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 69 273 40 56 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Glacier mass balance glacier modelling glacier volume mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Glacier mass balance glacier modelling glacier volume mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Daniel Falaschi Etienne Berthier Joaquín M. C. Belart Claudio Bravo Mariano Castro Marcelo Durand Ricardo Villalba Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
topic_facet |
Glacier mass balance glacier modelling glacier volume mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
We present geodetic mass-balance estimates for ten glaciers (22.6 ± 1.1 km2) around Volcán Domuyo between 1962 and 2020 (and 46 glaciers covering 29 ± 1.5 km2 between 1984 and 2020), derived from airborne, ASTER and Pléiades imagery. Overall, we find a slightly negative mass balance (−0.15 ± 0.09 m w.e. a–1) for the entire 1962–2020 time span. A closer inspection of sub-periods reveals, however, an increasingly negative mass balance with time. The Domuyo glaciers shifted from a moderately positive mass balance of +0.28 ± 0.13 m w.e. a–1 between 1962 and 1984, to a strongly negative mass balance of −0.99 ± 0.19 m w.e. a–1 between 2012 and 2020. An increase in summer temperatures and a decrease in winter precipitation during the last four decades are likely drivers of the observed glacier changes. We support this finding by implementing a minimal glacier model, relying solely on monthly precipitation and air temperatures. The mass-balance evolution detected in Volcán Domuyo is consistent with other sites spread across the Central Andes, suggesting rapidly increasing glacier wastage impacts are occurring at a geographically wider scale. |
format |
Article in Journal/Newspaper |
author |
Daniel Falaschi Etienne Berthier Joaquín M. C. Belart Claudio Bravo Mariano Castro Marcelo Durand Ricardo Villalba |
author_facet |
Daniel Falaschi Etienne Berthier Joaquín M. C. Belart Claudio Bravo Mariano Castro Marcelo Durand Ricardo Villalba |
author_sort |
Daniel Falaschi |
title |
Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
title_short |
Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
title_full |
Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
title_fullStr |
Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
title_full_unstemmed |
Increased mass loss of glaciers in Volcán Domuyo (Argentinian Andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
title_sort |
increased mass loss of glaciers in volcán domuyo (argentinian andes) between 1962 and 2020, revealed by aerial photos and satellite stereo imagery |
publisher |
Cambridge University Press |
publishDate |
2023 |
url |
https://doi.org/10.1017/jog.2022.43 https://doaj.org/article/7738ba1181564f04b027fb606aec69e6 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 69, Pp 40-56 (2023) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143022000430/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.43 0022-1430 1727-5652 https://doaj.org/article/7738ba1181564f04b027fb606aec69e6 |
op_doi |
https://doi.org/10.1017/jog.2022.43 |
container_title |
Journal of Glaciology |
container_volume |
69 |
container_issue |
273 |
container_start_page |
40 |
op_container_end_page |
56 |
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1766049112224956416 |