A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers

Achieving understanding and quantification of unknown aquifer systems in glacial context is crucial to forecast the evolution under climate change of water resources and of potential floods and landslides hazards. We focus on four south-eastern outlet glaciers of the main Icelandic icecap, Vatnajöku...

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Bibliographic Details
Main Authors: Vincent, Aude, Daigre, Clémence, Fischer, Ophélie, Aðalgeirsdóttir, Guðfinna, Violette, Sophie, Hart, Jane, Guðmundsson, Snævarr, Pálsson, Finnur
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1442
https://noa.gwlb.de/receive/cop_mods_00064521
https://egusphere.copernicus.org/preprints/egusphere-2022-1442/egusphere-2022-1442.pdf
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Summary:Achieving understanding and quantification of unknown aquifer systems in glacial context is crucial to forecast the evolution under climate change of water resources and of potential floods and landslides hazards. We focus on four south-eastern outlet glaciers of the main Icelandic icecap, Vatnajökull. New data are being acquired in the field to characterise groundwater dynamics. From this we propose a hydrogeological conceptual model: two distinct aquifers and their hydraulic conductivities are identified. A comprehensive water balance at the scale of the watershed has been obtained. Recharge to the aquifers is 4 times higher under the glaciers than on the plain, and we demonstrate the glacial melt recharge impact on the groundwater dynamic.