Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar

Source at https://doi.org/10.1017/jog.2018.54 . The phase-sensitive radio-echo sounder (pRES) is a powerful new instrument that can measure the depth of internal layers and the glacier bed to millimetre accuracy. We use a stationary 16-antenna pRES array on Store Glacier in West Greenland to measure...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Young, Tun Jan, Schroeder, Dustin M., Christoffersen, Poul, Lok, Lai B., Nicholls, Keith W., Brennan, Paul V., Doyle, Samuel H., Hubbard, Bryn, Hubbard, Alun Lloyd
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2018
Subjects:
Online Access:https://hdl.handle.net/10037/13609
https://doi.org/10.1017/jog.2018.54
id ftunivtroemsoe:oai:munin.uit.no:10037/13609
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/13609 2023-05-15T15:08:40+02:00 Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar Young, Tun Jan Schroeder, Dustin M. Christoffersen, Poul Lok, Lai B. Nicholls, Keith W. Brennan, Paul V. Doyle, Samuel H. Hubbard, Bryn Hubbard, Alun Lloyd 2018-07-19 https://hdl.handle.net/10037/13609 https://doi.org/10.1017/jog.2018.54 eng eng Cambridge University Press (CUP) Journal of Glaciology Young, T.J., Schroeder, P., Christoffersen, P., Lok, L.B., Nicholls, K.W., Brennan, P.V., . Hubbard, A.L. (2018). Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar. Journal of Glaciology, 64(246), 649-660. https://doi.org/10.1017/jog.2018.54 FRIDAID 1601340 doi:10.1017/jog.2018.54 0022-1430 1727-5652 https://hdl.handle.net/10037/13609 openAccess Arctic glaciology glaciological instruments and methods ground-penetrating radar radio-echo sounding VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 Journal article Tidsskriftartikkel Peer reviewed 2018 ftunivtroemsoe https://doi.org/10.1017/jog.2018.54 2021-06-25T17:56:02Z Source at https://doi.org/10.1017/jog.2018.54 . The phase-sensitive radio-echo sounder (pRES) is a powerful new instrument that can measure the depth of internal layers and the glacier bed to millimetre accuracy. We use a stationary 16-antenna pRES array on Store Glacier in West Greenland to measure the three-dimensional orientation of dipping internal reflectors, extending the capabilities of pRES beyond conventional depth sounding. This novel technique portrays the effectiveness of pRES in deriving the orientation of dipping internal layers that may complement profiles obtained through other geophysical surveying methods. Deriving ice vertical strain rates from changes in layer depth as measured by a sequence of pRES observations assumes that the internal reflections come from vertically beneath the antenna. By revealing the orientation of internal reflectors and the potential deviation from nadir of their associated reflections, the use of an antenna array can correct this assumption. While the array configuration was able to resolve the geometry of englacial layers, the same configuration could not be used to accurately image the glacier bed. Here, we use simulations of the performance of different array geometries to identify configurations that can be tailored to study different types of basal geometry for future deployments. Article in Journal/Newspaper Arctic glacier Greenland Journal of Glaciology University of Tromsø: Munin Open Research Archive Arctic Greenland Journal of Glaciology 64 246 649 660
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic Arctic glaciology
glaciological instruments and methods
ground-penetrating radar
radio-echo sounding
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
spellingShingle Arctic glaciology
glaciological instruments and methods
ground-penetrating radar
radio-echo sounding
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
Young, Tun Jan
Schroeder, Dustin M.
Christoffersen, Poul
Lok, Lai B.
Nicholls, Keith W.
Brennan, Paul V.
Doyle, Samuel H.
Hubbard, Bryn
Hubbard, Alun Lloyd
Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
topic_facet Arctic glaciology
glaciological instruments and methods
ground-penetrating radar
radio-echo sounding
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
description Source at https://doi.org/10.1017/jog.2018.54 . The phase-sensitive radio-echo sounder (pRES) is a powerful new instrument that can measure the depth of internal layers and the glacier bed to millimetre accuracy. We use a stationary 16-antenna pRES array on Store Glacier in West Greenland to measure the three-dimensional orientation of dipping internal reflectors, extending the capabilities of pRES beyond conventional depth sounding. This novel technique portrays the effectiveness of pRES in deriving the orientation of dipping internal layers that may complement profiles obtained through other geophysical surveying methods. Deriving ice vertical strain rates from changes in layer depth as measured by a sequence of pRES observations assumes that the internal reflections come from vertically beneath the antenna. By revealing the orientation of internal reflectors and the potential deviation from nadir of their associated reflections, the use of an antenna array can correct this assumption. While the array configuration was able to resolve the geometry of englacial layers, the same configuration could not be used to accurately image the glacier bed. Here, we use simulations of the performance of different array geometries to identify configurations that can be tailored to study different types of basal geometry for future deployments.
format Article in Journal/Newspaper
author Young, Tun Jan
Schroeder, Dustin M.
Christoffersen, Poul
Lok, Lai B.
Nicholls, Keith W.
Brennan, Paul V.
Doyle, Samuel H.
Hubbard, Bryn
Hubbard, Alun Lloyd
author_facet Young, Tun Jan
Schroeder, Dustin M.
Christoffersen, Poul
Lok, Lai B.
Nicholls, Keith W.
Brennan, Paul V.
Doyle, Samuel H.
Hubbard, Bryn
Hubbard, Alun Lloyd
author_sort Young, Tun Jan
title Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
title_short Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
title_full Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
title_fullStr Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
title_full_unstemmed Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
title_sort resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar
publisher Cambridge University Press (CUP)
publishDate 2018
url https://hdl.handle.net/10037/13609
https://doi.org/10.1017/jog.2018.54
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
glacier
Greenland
Journal of Glaciology
genre_facet Arctic
glacier
Greenland
Journal of Glaciology
op_relation Journal of Glaciology
Young, T.J., Schroeder, P., Christoffersen, P., Lok, L.B., Nicholls, K.W., Brennan, P.V., . Hubbard, A.L. (2018). Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar. Journal of Glaciology, 64(246), 649-660. https://doi.org/10.1017/jog.2018.54
FRIDAID 1601340
doi:10.1017/jog.2018.54
0022-1430
1727-5652
https://hdl.handle.net/10037/13609
op_rights openAccess
op_doi https://doi.org/10.1017/jog.2018.54
container_title Journal of Glaciology
container_volume 64
container_issue 246
container_start_page 649
op_container_end_page 660
_version_ 1766339983420948480