A stationary impulse-radar system for autonomous deployment in cold and temperate environments

Abstract Stationary ice-penetrating radar (sIPR) systems can be used to monitor temporal changes in electromagnetically sensitive properties of glaciers and ice sheets. We describe a system intended for autonomous operation in remote glacial environments, and document its performance during deployme...

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Published in:Annals of Glaciology
Main Authors: Mingo, Laurent, Flowers, Gwenn E., Crawford, Anna J., Mueller, Derek R., Bigelow, David G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2020
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2020.2
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000026
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spelling crcambridgeupr:10.1017/aog.2020.2 2024-06-23T07:45:36+00:00 A stationary impulse-radar system for autonomous deployment in cold and temperate environments Mingo, Laurent Flowers, Gwenn E. Crawford, Anna J. Mueller, Derek R. Bigelow, David G. 2020 http://dx.doi.org/10.1017/aog.2020.2 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000026 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by-nc-nd/4.0/ Annals of Glaciology volume 61, issue 81, page 99-107 ISSN 0260-3055 1727-5644 journal-article 2020 crcambridgeupr https://doi.org/10.1017/aog.2020.2 2024-05-29T08:09:18Z Abstract Stationary ice-penetrating radar (sIPR) systems can be used to monitor temporal changes in electromagnetically sensitive properties of glaciers and ice sheets. We describe a system intended for autonomous operation in remote glacial environments, and document its performance during deployments in cold and temperate settings. The design is patterned after an existing impulse radar system, with the addition of a fibre-optic link and timing module to control transmitter pulses, a micro-UPS (uninterruptable power supply) to prevent uncontrolled system shutdown and a customized satellite telemetry scheme. Various implementations of the sIPR were deployed on the Kaskawulsh Glacier near an ice-marginal lake in Yukon, Canada, for 44–77 days in summers 2014, 2015 and 2017. Pronounced perturbations to englacial radiostratigraphy were observed commensurate with lake filling and drainage, and are interpreted as changes in englacial water storage. Another sIPR was deployed in 2015–2016 on ice island PII-A-1-f, which originated from the Petermann Glacier in northwest Greenland. This system operated autonomously for almost a year during which changes in thickness of the ice column were clearly detected. Article in Journal/Newspaper Annals of Glaciology glacier glacier* Greenland Petermann glacier Yukon Cambridge University Press Yukon Canada Greenland Marginal Lake ENVELOPE(163.500,163.500,-74.600,-74.600) Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Annals of Glaciology 61 81 99 107
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Stationary ice-penetrating radar (sIPR) systems can be used to monitor temporal changes in electromagnetically sensitive properties of glaciers and ice sheets. We describe a system intended for autonomous operation in remote glacial environments, and document its performance during deployments in cold and temperate settings. The design is patterned after an existing impulse radar system, with the addition of a fibre-optic link and timing module to control transmitter pulses, a micro-UPS (uninterruptable power supply) to prevent uncontrolled system shutdown and a customized satellite telemetry scheme. Various implementations of the sIPR were deployed on the Kaskawulsh Glacier near an ice-marginal lake in Yukon, Canada, for 44–77 days in summers 2014, 2015 and 2017. Pronounced perturbations to englacial radiostratigraphy were observed commensurate with lake filling and drainage, and are interpreted as changes in englacial water storage. Another sIPR was deployed in 2015–2016 on ice island PII-A-1-f, which originated from the Petermann Glacier in northwest Greenland. This system operated autonomously for almost a year during which changes in thickness of the ice column were clearly detected.
format Article in Journal/Newspaper
author Mingo, Laurent
Flowers, Gwenn E.
Crawford, Anna J.
Mueller, Derek R.
Bigelow, David G.
spellingShingle Mingo, Laurent
Flowers, Gwenn E.
Crawford, Anna J.
Mueller, Derek R.
Bigelow, David G.
A stationary impulse-radar system for autonomous deployment in cold and temperate environments
author_facet Mingo, Laurent
Flowers, Gwenn E.
Crawford, Anna J.
Mueller, Derek R.
Bigelow, David G.
author_sort Mingo, Laurent
title A stationary impulse-radar system for autonomous deployment in cold and temperate environments
title_short A stationary impulse-radar system for autonomous deployment in cold and temperate environments
title_full A stationary impulse-radar system for autonomous deployment in cold and temperate environments
title_fullStr A stationary impulse-radar system for autonomous deployment in cold and temperate environments
title_full_unstemmed A stationary impulse-radar system for autonomous deployment in cold and temperate environments
title_sort stationary impulse-radar system for autonomous deployment in cold and temperate environments
publisher Cambridge University Press (CUP)
publishDate 2020
url http://dx.doi.org/10.1017/aog.2020.2
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000026
long_lat ENVELOPE(163.500,163.500,-74.600,-74.600)
ENVELOPE(-139.104,-139.104,60.749,60.749)
geographic Yukon
Canada
Greenland
Marginal Lake
Kaskawulsh Glacier
geographic_facet Yukon
Canada
Greenland
Marginal Lake
Kaskawulsh Glacier
genre Annals of Glaciology
glacier
glacier*
Greenland
Petermann glacier
Yukon
genre_facet Annals of Glaciology
glacier
glacier*
Greenland
Petermann glacier
Yukon
op_source Annals of Glaciology
volume 61, issue 81, page 99-107
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1017/aog.2020.2
container_title Annals of Glaciology
container_volume 61
container_issue 81
container_start_page 99
op_container_end_page 107
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