Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar
Ice penetrating radar (IPR) is a key tool in understanding the internal geometry and nature of glaciers and ice sheets, and has widely been used to derive bed topography, map internal layers and understand the thermal state of the cryosphere. Modern glacier and ice-sheet models facilitate increased...
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The University of Edinburgh
2021
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Online Access: | https://hdl.handle.net/1842/38123 https://doi.org/10.7488/era/1392 |
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ftunivedinburgh:oai:era.ed.ac.uk:1842/38123 2023-07-30T04:03:39+02:00 Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar Delf, Richard John Bingham, Robert Giannopoulos, Antonios Curtis, Andrew Nienow, Peter Natural Environment Research Council (NERC) 2021-07-31 application/pdf https://hdl.handle.net/1842/38123 https://doi.org/10.7488/era/1392 en eng The University of Edinburgh Delf, R., A. Giannopoulos, R. G. Bingham, N. R. Hulton, and A. Curtis (2017). “A Sliced-3D FDTD approach as an alternative to 2D Ground Penetrating Radar modelling”. In: 2017 9th International Workshop on Advanced Ground Penetrat ing Radar, IWAGPR 2017 - Proceedings. IEEE, pp. 1–5. isbn: 9781509054848. doi:10.1109/IWAGPR.2017.7996038. https://hdl.handle.net/1842/38123 http://dx.doi.org/10.7488/era/1392 glaciology geophysics ice penetrating radar glacier flow modelling Thesis or Dissertation Doctoral PhD Doctor of Philosophy 2021 ftunivedinburgh https://doi.org/10.7488/era/139210.1109/IWAGPR.2017.7996038 2023-07-09T20:29:14Z Ice penetrating radar (IPR) is a key tool in understanding the internal geometry and nature of glaciers and ice sheets, and has widely been used to derive bed topography, map internal layers and understand the thermal state of the cryosphere. Modern glacier and ice-sheet models facilitate increased assimilation of observations of englacial structure, including glacier thermal state and internal-layer geometry, yet the products available from radar surveys are often under-utilised. This thesis presents the development and assessment of radar processing strategies to improve quantitative retrievals from commonly acquired radar data. The first major focus of this thesis centres on deriving englacial velocities from zero-offset IPR data. Water held within micro- and macro-scale pores in ice has a direct influence on radar velocity, and significantly reduces ice viscosity and hence impacts the long-term evolution of polythermal glaciers. Knowledge of the radar velocity field is essential to retrieve correct bed topography from depth conversion processing, yet bed topography is often estimated assuming constant velocity, and potential errors from lateral variations in the velocity field are neglected. Here I calculate the englacial radar velocity field from common offset IPR data collected on Von Postbreen, a polythermal glacier in Svalbard. I first extract the diffracted wavefield using local coherent stacking, then use the focusing metric of negative entropy to deduce a local migration velocity field from constant-velocity migration panels and produce a glacier-wide model of local radar velocity. I show that this velocity field is successful in differentiating between areas of cold and temperate ice and can detect lateral variations in radar velocity close to the glacier bed. The effects of this velocity field in both migration and depth-conversion of the bed reflection are shown to result in consistently lower ice depths across the glacier, indicating that diffraction focusing and velocity estimation are crucial in ... Doctoral or Postdoctoral Thesis glacier Ice Sheet Svalbard Edinburgh Research Archive (ERA - University of Edinburgh) Svalbard Von Postbreen ENVELOPE(17.440,17.440,78.444,78.444) |
institution |
Open Polar |
collection |
Edinburgh Research Archive (ERA - University of Edinburgh) |
op_collection_id |
ftunivedinburgh |
language |
English |
topic |
glaciology geophysics ice penetrating radar glacier flow modelling |
spellingShingle |
glaciology geophysics ice penetrating radar glacier flow modelling Delf, Richard John Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
topic_facet |
glaciology geophysics ice penetrating radar glacier flow modelling |
description |
Ice penetrating radar (IPR) is a key tool in understanding the internal geometry and nature of glaciers and ice sheets, and has widely been used to derive bed topography, map internal layers and understand the thermal state of the cryosphere. Modern glacier and ice-sheet models facilitate increased assimilation of observations of englacial structure, including glacier thermal state and internal-layer geometry, yet the products available from radar surveys are often under-utilised. This thesis presents the development and assessment of radar processing strategies to improve quantitative retrievals from commonly acquired radar data. The first major focus of this thesis centres on deriving englacial velocities from zero-offset IPR data. Water held within micro- and macro-scale pores in ice has a direct influence on radar velocity, and significantly reduces ice viscosity and hence impacts the long-term evolution of polythermal glaciers. Knowledge of the radar velocity field is essential to retrieve correct bed topography from depth conversion processing, yet bed topography is often estimated assuming constant velocity, and potential errors from lateral variations in the velocity field are neglected. Here I calculate the englacial radar velocity field from common offset IPR data collected on Von Postbreen, a polythermal glacier in Svalbard. I first extract the diffracted wavefield using local coherent stacking, then use the focusing metric of negative entropy to deduce a local migration velocity field from constant-velocity migration panels and produce a glacier-wide model of local radar velocity. I show that this velocity field is successful in differentiating between areas of cold and temperate ice and can detect lateral variations in radar velocity close to the glacier bed. The effects of this velocity field in both migration and depth-conversion of the bed reflection are shown to result in consistently lower ice depths across the glacier, indicating that diffraction focusing and velocity estimation are crucial in ... |
author2 |
Bingham, Robert Giannopoulos, Antonios Curtis, Andrew Nienow, Peter Natural Environment Research Council (NERC) |
format |
Doctoral or Postdoctoral Thesis |
author |
Delf, Richard John |
author_facet |
Delf, Richard John |
author_sort |
Delf, Richard John |
title |
Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
title_short |
Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
title_full |
Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
title_fullStr |
Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
title_full_unstemmed |
Investigating the internal structure of glaciers and ice sheets using Ground Penetrating Radar |
title_sort |
investigating the internal structure of glaciers and ice sheets using ground penetrating radar |
publisher |
The University of Edinburgh |
publishDate |
2021 |
url |
https://hdl.handle.net/1842/38123 https://doi.org/10.7488/era/1392 |
long_lat |
ENVELOPE(17.440,17.440,78.444,78.444) |
geographic |
Svalbard Von Postbreen |
geographic_facet |
Svalbard Von Postbreen |
genre |
glacier Ice Sheet Svalbard |
genre_facet |
glacier Ice Sheet Svalbard |
op_relation |
Delf, R., A. Giannopoulos, R. G. Bingham, N. R. Hulton, and A. Curtis (2017). “A Sliced-3D FDTD approach as an alternative to 2D Ground Penetrating Radar modelling”. In: 2017 9th International Workshop on Advanced Ground Penetrat ing Radar, IWAGPR 2017 - Proceedings. IEEE, pp. 1–5. isbn: 9781509054848. doi:10.1109/IWAGPR.2017.7996038. https://hdl.handle.net/1842/38123 http://dx.doi.org/10.7488/era/1392 |
op_doi |
https://doi.org/10.7488/era/139210.1109/IWAGPR.2017.7996038 |
_version_ |
1772814697796468736 |