State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products
The glaciers of the Val Veny (Italian side of the Mont-Blanc Massif) have been the site of numerous field observations during the last decades, in particular for the study of glacial fluctuations or surface processes related to the debris cover. Here, we propose to examine how satellite observations...
Saved in:
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Institut de Géographie Alpine
2023-11-01
|
Series: | Revue de Géographie Alpine |
Subjects: | |
Online Access: | https://journals.openedition.org/rga/11619 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
_version_ | 1841546845211328512 |
---|---|
author | Antoine Rabatel Etienne Ducasse Victor Ramseyer Romain Millan |
author_facet | Antoine Rabatel Etienne Ducasse Victor Ramseyer Romain Millan |
author_sort | Antoine Rabatel |
collection | DOAJ |
description | The glaciers of the Val Veny (Italian side of the Mont-Blanc Massif) have been the site of numerous field observations during the last decades, in particular for the study of glacial fluctuations or surface processes related to the debris cover. Here, we propose to examine how satellite observations can complement field measurements on the state and fate of the Val Veny glaciers. Indeed, satellite products obtained in a quasi-systematic way allow to account not only for the loss of surface and volume, but also for the changes in their flow velocities. The overall pattern we document is a glacier thinning and slowdown of the ice flow, with an estimated shrinkage of 25% by 2050 and a volume loss ranging between 30 and 43% depending on the data source used for the estimation of the initial volume. In such a context, a portion of the upper reaches of Brenva Glacier shows an unexpected pattern of thickening and increase in ice flow that rises questions on its origin. Finally, the uncertainties in the estimation of ice thicknesses remain important and have repercussions on the future evolution of the glaciers and their contribution from a hydrological point of view. By 2050, we estimate that the water contribution due to the volume loss of Val Veny glaciers could decrease by 40%. |
format | Article |
id | doaj-art-e606c739c20c41e2a381306b15caf879 |
institution | Kabale University |
issn | 0035-1121 1760-7426 |
language | English |
publishDate | 2023-11-01 |
publisher | Institut de Géographie Alpine |
record_format | Article |
series | Revue de Géographie Alpine |
spelling | doaj-art-e606c739c20c41e2a381306b15caf8792025-01-10T15:53:57ZengInstitut de Géographie AlpineRevue de Géographie Alpine0035-11211760-74262023-11-01111210.4000/rga.11619State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite ProductsAntoine RabatelEtienne DucasseVictor RamseyerRomain MillanThe glaciers of the Val Veny (Italian side of the Mont-Blanc Massif) have been the site of numerous field observations during the last decades, in particular for the study of glacial fluctuations or surface processes related to the debris cover. Here, we propose to examine how satellite observations can complement field measurements on the state and fate of the Val Veny glaciers. Indeed, satellite products obtained in a quasi-systematic way allow to account not only for the loss of surface and volume, but also for the changes in their flow velocities. The overall pattern we document is a glacier thinning and slowdown of the ice flow, with an estimated shrinkage of 25% by 2050 and a volume loss ranging between 30 and 43% depending on the data source used for the estimation of the initial volume. In such a context, a portion of the upper reaches of Brenva Glacier shows an unexpected pattern of thickening and increase in ice flow that rises questions on its origin. Finally, the uncertainties in the estimation of ice thicknesses remain important and have repercussions on the future evolution of the glaciers and their contribution from a hydrological point of view. By 2050, we estimate that the water contribution due to the volume loss of Val Veny glaciers could decrease by 40%.https://journals.openedition.org/rga/11619European Alpsmountain glacierssurface area and volume changessatellite remote sensingVal Veny |
spellingShingle | Antoine Rabatel Etienne Ducasse Victor Ramseyer Romain Millan State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products Revue de Géographie Alpine European Alps mountain glaciers surface area and volume changes satellite remote sensing Val Veny |
title | State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products |
title_full | State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products |
title_fullStr | State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products |
title_full_unstemmed | State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products |
title_short | State and Fate of Glaciers in the Val Veny (Mont-Blanc Range, Italy): Contribution of Optical Satellite Products |
title_sort | state and fate of glaciers in the val veny mont blanc range italy contribution of optical satellite products |
topic | European Alps mountain glaciers surface area and volume changes satellite remote sensing Val Veny |
url | https://journals.openedition.org/rga/11619 |
work_keys_str_mv | AT antoinerabatel stateandfateofglaciersinthevalvenymontblancrangeitalycontributionofopticalsatelliteproducts AT etienneducasse stateandfateofglaciersinthevalvenymontblancrangeitalycontributionofopticalsatelliteproducts AT victorramseyer stateandfateofglaciersinthevalvenymontblancrangeitalycontributionofopticalsatelliteproducts AT romainmillan stateandfateofglaciersinthevalvenymontblancrangeitalycontributionofopticalsatelliteproducts |