Radio Echo Sounding On Temperate Glaciers

A high-resolution radio echo sounder operating at a frequency of 620 MHz has been developed for studies of temperate glaciers. Excellent spatial resolution is obtained through the use of a short pulse length (70 ns) and an antenna beam width of 5.2°. Large amounts of high-quality data may be rapidly...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Goodman, R. H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000013393
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013393
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spelling crcambridgeupr:10.1017/s0022143000013393 2024-03-03T08:46:04+00:00 Radio Echo Sounding On Temperate Glaciers Goodman, R. H. 1975 http://dx.doi.org/10.1017/s0022143000013393 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013393 en eng Cambridge University Press (CUP) Journal of Glaciology volume 14, issue 70, page 57-69 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000013393 2024-02-08T08:42:50Z A high-resolution radio echo sounder operating at a frequency of 620 MHz has been developed for studies of temperate glaciers. Excellent spatial resolution is obtained through the use of a short pulse length (70 ns) and an antenna beam width of 5.2°. Large amounts of high-quality data may be rapidly collected since the sounder incorporates an automatic positioning system and an on-line computer. Real time analysis of the echoes facilitates the understanding of complex reflecting horizons observed in temperate glaciers. Results obtained during field trials of the echo sounder on both the Wapta Icefield and Athabasca Glacier are given. Intraglacial structures which may be due to water levels within the ice have been detected. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 14 70 57 69
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Goodman, R. H.
Radio Echo Sounding On Temperate Glaciers
topic_facet Earth-Surface Processes
description A high-resolution radio echo sounder operating at a frequency of 620 MHz has been developed for studies of temperate glaciers. Excellent spatial resolution is obtained through the use of a short pulse length (70 ns) and an antenna beam width of 5.2°. Large amounts of high-quality data may be rapidly collected since the sounder incorporates an automatic positioning system and an on-line computer. Real time analysis of the echoes facilitates the understanding of complex reflecting horizons observed in temperate glaciers. Results obtained during field trials of the echo sounder on both the Wapta Icefield and Athabasca Glacier are given. Intraglacial structures which may be due to water levels within the ice have been detected.
format Article in Journal/Newspaper
author Goodman, R. H.
author_facet Goodman, R. H.
author_sort Goodman, R. H.
title Radio Echo Sounding On Temperate Glaciers
title_short Radio Echo Sounding On Temperate Glaciers
title_full Radio Echo Sounding On Temperate Glaciers
title_fullStr Radio Echo Sounding On Temperate Glaciers
title_full_unstemmed Radio Echo Sounding On Temperate Glaciers
title_sort radio echo sounding on temperate glaciers
publisher Cambridge University Press (CUP)
publishDate 1975
url http://dx.doi.org/10.1017/s0022143000013393
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013393
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 14, issue 70, page 57-69
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000013393
container_title Journal of Glaciology
container_volume 14
container_issue 70
container_start_page 57
op_container_end_page 69
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