Ground-penetrating radar imaging reveals glacier's drainage network in 3D
Hydrological systems of glaciers have a direct impact on the glacier dynamics. Since the 1950s, geophysical studies have provided insights into these hydrological systems. Unfortunately, such studies were predominantly conducted using 2D acquisitions along a few profiles, thus failing to provide spa...
Main Authors: | , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus
2021
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/504095 https://doi.org/10.3929/ethz-b-000504095 |
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author | Church, Gregory James id_orcid:0 000-0003-0114-9950 Bauder, Andreas id_orcid:0 000-0001-7197-7706 Grab, Melchior id_orcid:0 000-0002-8293-4872 Maurer, Hansruedi |
author_facet | Church, Gregory James id_orcid:0 000-0003-0114-9950 Bauder, Andreas id_orcid:0 000-0001-7197-7706 Grab, Melchior id_orcid:0 000-0002-8293-4872 Maurer, Hansruedi |
author_sort | Church, Gregory James |
collection | ETH Zürich Research Collection |
description | Hydrological systems of glaciers have a direct impact on the glacier dynamics. Since the 1950s, geophysical studies have provided insights into these hydrological systems. Unfortunately, such studies were predominantly conducted using 2D acquisitions along a few profiles, thus failing to provide spatially unaliased 3D images of englacial and subglacial water pathways. The latter has likely resulted in flawed constraints for the hydrological modelling of glacier drainage networks. Here, we present 3D ground-penetrating radar (GPR) results that provide high-resolution 3D images of an alpine glacier's drainage network. Our results confirm a long-standing englacial hydrology theory stating that englacial conduits flow around glacial overdeepenings rather than directly over the overdeepening. Furthermore, these results also show exciting new opportunities for highresolution 3D GPR studies of glaciers. ISSN:1994-0416 ISSN:1994-0424 |
format | Article in Journal/Newspaper |
genre | The Cryosphere |
genre_facet | The Cryosphere |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/504095 |
institution | Open Polar |
language | English |
op_collection_id | ftethz |
op_doi | https://doi.org/20.500.11850/50409510.3929/ethz-b-00050409510.5194/tc-15-3975-2021 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-3975-2021 info:eu-repo/semantics/altIdentifier/wos/000688081700001 info:eu-repo/grantAgreement/SNF/Projekte MINT/169329 http://hdl.handle.net/20.500.11850/504095 |
op_rights | info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International |
op_source | The Cryosphere, 15 (8) |
publishDate | 2021 |
publisher | Copernicus |
record_format | openpolar |
spelling | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/504095 2025-03-30T15:28:58+00:00 Ground-penetrating radar imaging reveals glacier's drainage network in 3D Church, Gregory James id_orcid:0 000-0003-0114-9950 Bauder, Andreas id_orcid:0 000-0001-7197-7706 Grab, Melchior id_orcid:0 000-0002-8293-4872 Maurer, Hansruedi 2021-08-23 application/application/pdf https://hdl.handle.net/20.500.11850/504095 https://doi.org/10.3929/ethz-b-000504095 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-3975-2021 info:eu-repo/semantics/altIdentifier/wos/000688081700001 info:eu-repo/grantAgreement/SNF/Projekte MINT/169329 http://hdl.handle.net/20.500.11850/504095 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International The Cryosphere, 15 (8) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftethz https://doi.org/20.500.11850/50409510.3929/ethz-b-00050409510.5194/tc-15-3975-2021 2025-03-05T22:09:14Z Hydrological systems of glaciers have a direct impact on the glacier dynamics. Since the 1950s, geophysical studies have provided insights into these hydrological systems. Unfortunately, such studies were predominantly conducted using 2D acquisitions along a few profiles, thus failing to provide spatially unaliased 3D images of englacial and subglacial water pathways. The latter has likely resulted in flawed constraints for the hydrological modelling of glacier drainage networks. Here, we present 3D ground-penetrating radar (GPR) results that provide high-resolution 3D images of an alpine glacier's drainage network. Our results confirm a long-standing englacial hydrology theory stating that englacial conduits flow around glacial overdeepenings rather than directly over the overdeepening. Furthermore, these results also show exciting new opportunities for highresolution 3D GPR studies of glaciers. ISSN:1994-0416 ISSN:1994-0424 Article in Journal/Newspaper The Cryosphere ETH Zürich Research Collection |
spellingShingle | Church, Gregory James id_orcid:0 000-0003-0114-9950 Bauder, Andreas id_orcid:0 000-0001-7197-7706 Grab, Melchior id_orcid:0 000-0002-8293-4872 Maurer, Hansruedi Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title | Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title_full | Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title_fullStr | Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title_full_unstemmed | Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title_short | Ground-penetrating radar imaging reveals glacier's drainage network in 3D |
title_sort | ground-penetrating radar imaging reveals glacier's drainage network in 3d |
url | https://hdl.handle.net/20.500.11850/504095 https://doi.org/10.3929/ethz-b-000504095 |