Radio Echo-Sounding of Svalbard Glaciers
Abstract Peculiarities of radio echo-sounding of mountain glaciers and ice fields between nunataks from terrestrial vehicles and from helicopters are considered in this paper. The possibility of using comparatively high frequencies (of up to 865 MHz) for sounding such glaciers is demonstrated on the...
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Language: | English |
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Cambridge University Press (CUP)
1982
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Online Access: | http://dx.doi.org/10.1017/s0022143000011643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011643 |
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crcambridgeupr:10.1017/s0022143000011643 2024-09-15T18:07:55+00:00 Radio Echo-Sounding of Svalbard Glaciers Macheret, Yu. Ya. Zhuravlev, A. B. 1982 http://dx.doi.org/10.1017/s0022143000011643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011643 en eng Cambridge University Press (CUP) Journal of Glaciology volume 28, issue 99, page 295-314 ISSN 0022-1430 1727-5652 journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0022143000011643 2024-07-24T04:02:42Z Abstract Peculiarities of radio echo-sounding of mountain glaciers and ice fields between nunataks from terrestrial vehicles and from helicopters are considered in this paper. The possibility of using comparatively high frequencies (of up to 865 MHz) for sounding such glaciers is demonstrated on the basis of experimental data. Results of airborne radio echo-sounding of Svalbard glaciers of various types, dimensions, and regime obtained with the help of the 620 MHz airborne equipment of high resolution are shown. Returns from the glacier bed have been obtained on the majority of glaciers under investigation. The firn regions of ice fields with temperate regimes flowing between nunataks are, mostly, an exception. Depression in the glacier bed with the ice thickness up to 540 m, as well as internal reflecting boundaries have been detected in some glaciers. Ice volumes of glaciers have been determined from the airborne radio echo-sounding data with the use of a parabolic approximation to the cross-section glacier profiles. Good correlational dependence between ice volume and surface area of glaciers has been established and is used to estimate the ice and water resources in Svalbard glaciers. Article in Journal/Newspaper glacier Journal of Glaciology Svalbard Cambridge University Press Journal of Glaciology 28 99 295 314 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract Peculiarities of radio echo-sounding of mountain glaciers and ice fields between nunataks from terrestrial vehicles and from helicopters are considered in this paper. The possibility of using comparatively high frequencies (of up to 865 MHz) for sounding such glaciers is demonstrated on the basis of experimental data. Results of airborne radio echo-sounding of Svalbard glaciers of various types, dimensions, and regime obtained with the help of the 620 MHz airborne equipment of high resolution are shown. Returns from the glacier bed have been obtained on the majority of glaciers under investigation. The firn regions of ice fields with temperate regimes flowing between nunataks are, mostly, an exception. Depression in the glacier bed with the ice thickness up to 540 m, as well as internal reflecting boundaries have been detected in some glaciers. Ice volumes of glaciers have been determined from the airborne radio echo-sounding data with the use of a parabolic approximation to the cross-section glacier profiles. Good correlational dependence between ice volume and surface area of glaciers has been established and is used to estimate the ice and water resources in Svalbard glaciers. |
format |
Article in Journal/Newspaper |
author |
Macheret, Yu. Ya. Zhuravlev, A. B. |
spellingShingle |
Macheret, Yu. Ya. Zhuravlev, A. B. Radio Echo-Sounding of Svalbard Glaciers |
author_facet |
Macheret, Yu. Ya. Zhuravlev, A. B. |
author_sort |
Macheret, Yu. Ya. |
title |
Radio Echo-Sounding of Svalbard Glaciers |
title_short |
Radio Echo-Sounding of Svalbard Glaciers |
title_full |
Radio Echo-Sounding of Svalbard Glaciers |
title_fullStr |
Radio Echo-Sounding of Svalbard Glaciers |
title_full_unstemmed |
Radio Echo-Sounding of Svalbard Glaciers |
title_sort |
radio echo-sounding of svalbard glaciers |
publisher |
Cambridge University Press (CUP) |
publishDate |
1982 |
url |
http://dx.doi.org/10.1017/s0022143000011643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011643 |
genre |
glacier Journal of Glaciology Svalbard |
genre_facet |
glacier Journal of Glaciology Svalbard |
op_source |
Journal of Glaciology volume 28, issue 99, page 295-314 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000011643 |
container_title |
Journal of Glaciology |
container_volume |
28 |
container_issue |
99 |
container_start_page |
295 |
op_container_end_page |
314 |
_version_ |
1810445281995522048 |