Articles | Volume 14, issue 10
https://doi.org/10.5194/tc-14-3269-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-3269-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
02 Oct 2020
Research article |
| 02 Oct 2020
| 02 Oct 2020
Monitoring the seasonal changes of an englacial conduit network using repeated ground-penetrating radar measurements
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, Switzerland
Institute of Geophysics, ETH Zurich, Zurich, Switzerland
Invited contribution by Gregory Church, recipient of the EGU Cryospheric Sciences Outstanding Student Poster and PICO Award 2019.
Melchior Grab
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, Switzerland
Institute of Geophysics, ETH Zurich, Zurich, Switzerland
Cédric Schmelzbach
Institute of Geophysics, ETH Zurich, Zurich, Switzerland
Andreas Bauder
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, Switzerland
Hansruedi Maurer
Institute of Geophysics, ETH Zurich, Zurich, Switzerland
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Cited
17 citations as recorded by crossref.
- Diurnal expansion and contraction of englacial fracture networks revealed by seismic shear wave splitting W. Gajek et al. 10.1038/s43247-021-00279-4
- Characterization of subglacial marginal channels using 3-D analysis of high-density ground-penetrating radar data P. Egli et al. 10.1017/jog.2021.26
- Glacial hydraulic tremor on Rhonegletscher, Switzerland E. Clyne et al. 10.1017/jog.2022.69
- Development of a drone-based ground-penetrating radar system for efficient and safe 3D and 4D surveying of alpine glaciers B. Ruols et al. 10.1017/jog.2023.83
- Strong MARSIS Radar Reflections From the Base of Martian South Polar Cap May Be Due to Conductive Ice or Minerals C. Bierson et al. 10.1029/2021GL093880
- Ground penetrating radar in temperate ice: englacial water inclusions as limiting factor for data interpretation C. Ogier et al. 10.1017/jog.2023.68
- Geophysical constraints on the properties of a subglacial lake in northwest Greenland R. Maguire et al. 10.5194/tc-15-3279-2021
- The role of electrical conductivity in radar wave reflection from glacier beds S. Tulaczyk & N. Foley 10.5194/tc-14-4495-2020
- Controls on Greenland moulin geometry and evolution from the Moulin Shape model L. Andrews et al. 10.5194/tc-16-2421-2022
- Paths forward in radioglaciology D. Schroeder 10.1017/aog.2023.3
- A borehole trajectory inversion scheme to adjust the measurement geometry for 3D travel-time tomography on glaciers S. Hellmann et al. 10.5194/se-14-805-2023
- The evolution and preservation potential of englacial eskers: An example from Breiðamerkurjökull, SE Iceland A. Lally et al. 10.1002/esp.5664
- Ground-penetrating radar imaging reveals glacier's drainage network in 3D G. Church et al. 10.5194/tc-15-3975-2021
- Development of a workflow for processing ground-penetrating radar data from multiconcurrent receivers D. Angelis et al. 10.1190/geo2021-0376.1
- Topology and spatial-pressure-distribution reconstruction of an englacial channel L. Piho et al. 10.5194/tc-16-3669-2022
- Evidences of Bedrock Forcing on Glacier Morphodynamics: A Case Study in Italian Alps N. Dematteis et al. 10.3389/feart.2022.793546
- Investigating the Radar Response of Englacial Debris Entrained Basal Ice Units in East Antarctica Using Electromagnetic Forward Modeling S. Franke et al. 10.1109/TGRS.2023.3277874
17 citations as recorded by crossref.
- Diurnal expansion and contraction of englacial fracture networks revealed by seismic shear wave splitting W. Gajek et al. 10.1038/s43247-021-00279-4
- Characterization of subglacial marginal channels using 3-D analysis of high-density ground-penetrating radar data P. Egli et al. 10.1017/jog.2021.26
- Glacial hydraulic tremor on Rhonegletscher, Switzerland E. Clyne et al. 10.1017/jog.2022.69
- Development of a drone-based ground-penetrating radar system for efficient and safe 3D and 4D surveying of alpine glaciers B. Ruols et al. 10.1017/jog.2023.83
- Strong MARSIS Radar Reflections From the Base of Martian South Polar Cap May Be Due to Conductive Ice or Minerals C. Bierson et al. 10.1029/2021GL093880
- Ground penetrating radar in temperate ice: englacial water inclusions as limiting factor for data interpretation C. Ogier et al. 10.1017/jog.2023.68
- Geophysical constraints on the properties of a subglacial lake in northwest Greenland R. Maguire et al. 10.5194/tc-15-3279-2021
- The role of electrical conductivity in radar wave reflection from glacier beds S. Tulaczyk & N. Foley 10.5194/tc-14-4495-2020
- Controls on Greenland moulin geometry and evolution from the Moulin Shape model L. Andrews et al. 10.5194/tc-16-2421-2022
- Paths forward in radioglaciology D. Schroeder 10.1017/aog.2023.3
- A borehole trajectory inversion scheme to adjust the measurement geometry for 3D travel-time tomography on glaciers S. Hellmann et al. 10.5194/se-14-805-2023
- The evolution and preservation potential of englacial eskers: An example from Breiðamerkurjökull, SE Iceland A. Lally et al. 10.1002/esp.5664
- Ground-penetrating radar imaging reveals glacier's drainage network in 3D G. Church et al. 10.5194/tc-15-3975-2021
- Development of a workflow for processing ground-penetrating radar data from multiconcurrent receivers D. Angelis et al. 10.1190/geo2021-0376.1
- Topology and spatial-pressure-distribution reconstruction of an englacial channel L. Piho et al. 10.5194/tc-16-3669-2022
- Evidences of Bedrock Forcing on Glacier Morphodynamics: A Case Study in Italian Alps N. Dematteis et al. 10.3389/feart.2022.793546
- Investigating the Radar Response of Englacial Debris Entrained Basal Ice Units in East Antarctica Using Electromagnetic Forward Modeling S. Franke et al. 10.1109/TGRS.2023.3277874
Latest update: 18 Apr 2024
Short summary
In this field study, we repeated ground-penetrating radar measurements over an active englacial channel network that transports meltwater through the glacier. We successfully imaged the englacial meltwater pathway and were able to delimitate the channel's shape. Meltwater from the glacier can impact the glacier's dynamics if it reaches the ice–bed interface, and therefore monitoring these englacial drainage networks is important to understand how these networks behave throughout a season.
In this field study, we repeated ground-penetrating radar measurements over an active englacial...
