Ground-penetrating radar imaging reveals glacier's drainage network in 3D

<p>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 pr...

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Main Authors: G. Church, A. Bauder, M. Grab, H. Maurer
Format: Article
Language:English
Published: Copernicus Publications 2021-08-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/15/3975/2021/tc-15-3975-2021.pdf
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spelling doaj-bede2abd6773426fb87af0fb84e719f22021-08-23T08:33:05ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242021-08-01153975398810.5194/tc-15-3975-2021Ground-penetrating radar imaging reveals glacier's drainage network in 3DG. Church0G. Church1A. Bauder2M. Grab3M. Grab4H. Maurer5Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, SwitzerlandInstitute of Geophysics, ETH Zurich, Zurich, SwitzerlandLaboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, SwitzerlandLaboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, SwitzerlandInstitute of Geophysics, ETH Zurich, Zurich, SwitzerlandInstitute of Geophysics, ETH Zurich, Zurich, Switzerland<p>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 high-resolution 3D GPR studies of glaciers.</p>https://tc.copernicus.org/articles/15/3975/2021/tc-15-3975-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. Church
G. Church
A. Bauder
M. Grab
M. Grab
H. Maurer
spellingShingle G. Church
G. Church
A. Bauder
M. Grab
M. Grab
H. Maurer
Ground-penetrating radar imaging reveals glacier's drainage network in 3D
The Cryosphere
author_facet G. Church
G. Church
A. Bauder
M. Grab
M. Grab
H. Maurer
author_sort G. Church
title 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_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_sort ground-penetrating radar imaging reveals glacier's drainage network in 3d
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2021-08-01
description <p>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 high-resolution 3D GPR studies of glaciers.</p>
url https://tc.copernicus.org/articles/15/3975/2021/tc-15-3975-2021.pdf
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