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

For reliable forecasting of the evolution of critical water resources, as well as of potential flood and landslide hazards and their response to climate change, it is necessary to improve the understanding and quantification of unknown aquifer systems in glacierized catchments. We focus on four sout...

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Published in:Hydrology and Earth System Sciences
Main Authors: Vincent, Aude, Daigre, Clémence, Fischer, Ophélie, Aðalgeirsdóttir, Guðfinna, Violette, Sophie, Hart, Jane, Guðmundsson, Snævarr, Pálsson, Finnur
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/hess-28-3475-2024
https://hess.copernicus.org/articles/28/3475/2024/
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spelling ftcopernicus:oai:publications.copernicus.org:hess108423 2024-09-15T18:11:47+00:00 A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers Vincent, Aude Daigre, Clémence Fischer, Ophélie Aðalgeirsdóttir, Guðfinna Violette, Sophie Hart, Jane Guðmundsson, Snævarr Pálsson, Finnur 2024-07-31 application/pdf https://doi.org/10.5194/hess-28-3475-2024 https://hess.copernicus.org/articles/28/3475/2024/ eng eng doi:10.5194/hess-28-3475-2024 https://hess.copernicus.org/articles/28/3475/2024/ eISSN: 1607-7938 Text 2024 ftcopernicus https://doi.org/10.5194/hess-28-3475-2024 2024-08-05T14:04:48Z For reliable forecasting of the evolution of critical water resources, as well as of potential flood and landslide hazards and their response to climate change, it is necessary to improve the understanding and quantification of unknown aquifer systems in glacierized catchments. We focus on four southeastern outlet glaciers of the main Icelandic ice cap, Vatnajökull. A multidisciplinary approach is carried out, including the acquisition of new in situ data to characterize aquifers and their groundwater dynamics. Moreover, the recharge to aquifers from glacial melt and effective rainfall is estimated. From a detailed analysis of all available data and the determination of the dynamic characteristics of the aquifers, a hydrogeological conceptual model of glacierized catchments is constructed: (i) two distinct aquifers, their hydraulic conductivities and their hydrodynamic responses to climate forcing are identified; (ii) a comprehensive water balance for the whole catchment is obtained; (iii) the subglacial recharge to the aquifers is shown to be 4 times higher than in the proglacial area; and (v) the importance of the impact of the glacial melt recharge on the groundwater system is demonstrated. Thus, we highlight the major role that the groundwater component has in the hydrodynamic functioning of glacierized catchments. Text Ice cap Vatnajökull Copernicus Publications: E-Journals Hydrology and Earth System Sciences 28 14 3475 3494
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collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description For reliable forecasting of the evolution of critical water resources, as well as of potential flood and landslide hazards and their response to climate change, it is necessary to improve the understanding and quantification of unknown aquifer systems in glacierized catchments. We focus on four southeastern outlet glaciers of the main Icelandic ice cap, Vatnajökull. A multidisciplinary approach is carried out, including the acquisition of new in situ data to characterize aquifers and their groundwater dynamics. Moreover, the recharge to aquifers from glacial melt and effective rainfall is estimated. From a detailed analysis of all available data and the determination of the dynamic characteristics of the aquifers, a hydrogeological conceptual model of glacierized catchments is constructed: (i) two distinct aquifers, their hydraulic conductivities and their hydrodynamic responses to climate forcing are identified; (ii) a comprehensive water balance for the whole catchment is obtained; (iii) the subglacial recharge to the aquifers is shown to be 4 times higher than in the proglacial area; and (v) the importance of the impact of the glacial melt recharge on the groundwater system is demonstrated. Thus, we highlight the major role that the groundwater component has in the hydrodynamic functioning of glacierized catchments.
format Text
author Vincent, Aude
Daigre, Clémence
Fischer, Ophélie
Aðalgeirsdóttir, Guðfinna
Violette, Sophie
Hart, Jane
Guðmundsson, Snævarr
Pálsson, Finnur
spellingShingle Vincent, Aude
Daigre, Clémence
Fischer, Ophélie
Aðalgeirsdóttir, Guðfinna
Violette, Sophie
Hart, Jane
Guðmundsson, Snævarr
Pálsson, Finnur
A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
author_facet Vincent, Aude
Daigre, Clémence
Fischer, Ophélie
Aðalgeirsdóttir, Guðfinna
Violette, Sophie
Hart, Jane
Guðmundsson, Snævarr
Pálsson, Finnur
author_sort Vincent, Aude
title A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
title_short A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
title_full A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
title_fullStr A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
title_full_unstemmed A hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
title_sort hydrogeological conceptual model of aquifers in catchments headed by temperate glaciers
publishDate 2024
url https://doi.org/10.5194/hess-28-3475-2024
https://hess.copernicus.org/articles/28/3475/2024/
genre Ice cap
Vatnajökull
genre_facet Ice cap
Vatnajökull
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-28-3475-2024
https://hess.copernicus.org/articles/28/3475/2024/
op_doi https://doi.org/10.5194/hess-28-3475-2024
container_title Hydrology and Earth System Sciences
container_volume 28
container_issue 14
container_start_page 3475
op_container_end_page 3494
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