Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry
Abstract A major question in ice-sheet dynamics is the state of balance between the net mass input and ice flow. Since an imbalance produces a change in surface elevation, the state of balance can be studied by monitoring the elevation, and this has been accomplished by surface-leveling techniques i...
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Cambridge University Press (CUP)
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Online Access: | http://dx.doi.org/10.1017/s0022143000015045 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015045 |
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crcambridgeupr:10.1017/s0022143000015045 2024-03-03T08:45:01+00:00 Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry Zwally, H. Jay Brooks, R. L. Stanley, H. Ray Campbell, W. J. 1979 http://dx.doi.org/10.1017/s0022143000015045 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015045 en eng Cambridge University Press (CUP) Journal of Glaciology volume 24, issue 90, page 491-493 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000015045 2024-02-08T08:41:37Z Abstract A major question in ice-sheet dynamics is the state of balance between the net mass input and ice flow. Since an imbalance produces a change in surface elevation, the state of balance can be studied by monitoring the elevation, and this has been accomplished by surface-leveling techniques in a few locations. Due to the requirement for accurate and repetitive measurements over large areas, it is not practical to determine the status of balance of an entire ice sheet or even a major drainage basin by conventional techniques. Now, recent results from satellite-borne radar altimeter measurements over the Greenland ice sheet demonstrate the feasibility of accurately measuring and monitoring the topography of large ice masses. The application of this new technique offers the possibility of making a meaningful mass-balance determination and for detecting actual or potential ice-sheet surges. Article in Journal/Newspaper Greenland Ice Sheet Journal of Glaciology Cambridge University Press Greenland Journal of Glaciology 24 90 491 493 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Zwally, H. Jay Brooks, R. L. Stanley, H. Ray Campbell, W. J. Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
topic_facet |
Earth-Surface Processes |
description |
Abstract A major question in ice-sheet dynamics is the state of balance between the net mass input and ice flow. Since an imbalance produces a change in surface elevation, the state of balance can be studied by monitoring the elevation, and this has been accomplished by surface-leveling techniques in a few locations. Due to the requirement for accurate and repetitive measurements over large areas, it is not practical to determine the status of balance of an entire ice sheet or even a major drainage basin by conventional techniques. Now, recent results from satellite-borne radar altimeter measurements over the Greenland ice sheet demonstrate the feasibility of accurately measuring and monitoring the topography of large ice masses. The application of this new technique offers the possibility of making a meaningful mass-balance determination and for detecting actual or potential ice-sheet surges. |
format |
Article in Journal/Newspaper |
author |
Zwally, H. Jay Brooks, R. L. Stanley, H. Ray Campbell, W. J. |
author_facet |
Zwally, H. Jay Brooks, R. L. Stanley, H. Ray Campbell, W. J. |
author_sort |
Zwally, H. Jay |
title |
Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
title_short |
Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
title_full |
Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
title_fullStr |
Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
title_full_unstemmed |
Ice-Sheet Surface Elevation and Changes Observable by Satellite Radar Altimetry |
title_sort |
ice-sheet surface elevation and changes observable by satellite radar altimetry |
publisher |
Cambridge University Press (CUP) |
publishDate |
1979 |
url |
http://dx.doi.org/10.1017/s0022143000015045 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015045 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet Journal of Glaciology |
genre_facet |
Greenland Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 24, issue 90, page 491-493 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000015045 |
container_title |
Journal of Glaciology |
container_volume |
24 |
container_issue |
90 |
container_start_page |
491 |
op_container_end_page |
493 |
_version_ |
1792500529454120960 |