Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry
Abstract The synthetic-aperture radar-interferometry technique is used to detect the migration of the limit of tidal flexing, or hinge line, of the floating ice longue of Peter-mann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automatically from differential inter...
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1998
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Online Access: | http://dx.doi.org/10.1017/s0022143000001994 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001994 |
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crcambridgeupr:10.1017/s0022143000001994 2024-06-23T07:53:01+00:00 Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry Rignot, Eric 1998 http://dx.doi.org/10.1017/s0022143000001994 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001994 en eng Cambridge University Press (CUP) Journal of Glaciology volume 44, issue 148, page 469-476 ISSN 0022-1430 1727-5652 journal-article 1998 crcambridgeupr https://doi.org/10.1017/s0022143000001994 2024-06-05T04:04:05Z Abstract The synthetic-aperture radar-interferometry technique is used to detect the migration of the limit of tidal flexing, or hinge line, of the floating ice longue of Peter-mann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automatically from differential interferograms using a model-fitting technique based on an elastic-beam theory. The statistical noise of the model fit is less than 3 mm, and the hinge line is mapped with a precision of 30 m. Following automatic registration of multidate image data to a precision of 5m, hinge-line migration is subsequently detected with a precision of 40 m in the horizontal plane across the glacier width. The results show that the hinge line of Petermann Gletscher migrates back and forth with tide by ±70m, in excellent agreement with the migration calculated from ocean tides predicted by a tidal model combined with the glacier surface and basal slope measured by an ice-sounding radar. Superimposed on the short-term hinge-line migration due to tide, we detect a hinge-line retreat of 270 m in 3.87 years which varies across the glacier width by ± 120 m. The retreat suggests glacier thinning at a rate of 78 + 35 cm ice a −1 . Coincidentally, an analysis of ice-volume fluxes indicates that the hinge-line ice flux of Petermann Gletscher exceeds its balance flux by 0.88±1km 3 ice a −1 , which in turn implies glacier thinning at 83+95cm ice a −1 in the glacier lower reaches. Both methods therefore suggest that Petermann Gletscher is currently losing mass to the ocean. Article in Journal/Newspaper glacier Greenland Journal of Glaciology North Greenland Petermann gletscher Cambridge University Press Greenland Petermann Gletscher ENVELOPE(-59.500,-59.500,80.500,80.500) Journal of Glaciology 44 148 469 476 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract The synthetic-aperture radar-interferometry technique is used to detect the migration of the limit of tidal flexing, or hinge line, of the floating ice longue of Peter-mann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automatically from differential interferograms using a model-fitting technique based on an elastic-beam theory. The statistical noise of the model fit is less than 3 mm, and the hinge line is mapped with a precision of 30 m. Following automatic registration of multidate image data to a precision of 5m, hinge-line migration is subsequently detected with a precision of 40 m in the horizontal plane across the glacier width. The results show that the hinge line of Petermann Gletscher migrates back and forth with tide by ±70m, in excellent agreement with the migration calculated from ocean tides predicted by a tidal model combined with the glacier surface and basal slope measured by an ice-sounding radar. Superimposed on the short-term hinge-line migration due to tide, we detect a hinge-line retreat of 270 m in 3.87 years which varies across the glacier width by ± 120 m. The retreat suggests glacier thinning at a rate of 78 + 35 cm ice a −1 . Coincidentally, an analysis of ice-volume fluxes indicates that the hinge-line ice flux of Petermann Gletscher exceeds its balance flux by 0.88±1km 3 ice a −1 , which in turn implies glacier thinning at 83+95cm ice a −1 in the glacier lower reaches. Both methods therefore suggest that Petermann Gletscher is currently losing mass to the ocean. |
format |
Article in Journal/Newspaper |
author |
Rignot, Eric |
spellingShingle |
Rignot, Eric Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
author_facet |
Rignot, Eric |
author_sort |
Rignot, Eric |
title |
Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
title_short |
Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
title_full |
Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
title_fullStr |
Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
title_full_unstemmed |
Hinge-line migration of Petermann Gletscher, north Greenland, detected using satellite-radar interferometry |
title_sort |
hinge-line migration of petermann gletscher, north greenland, detected using satellite-radar interferometry |
publisher |
Cambridge University Press (CUP) |
publishDate |
1998 |
url |
http://dx.doi.org/10.1017/s0022143000001994 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001994 |
long_lat |
ENVELOPE(-59.500,-59.500,80.500,80.500) |
geographic |
Greenland Petermann Gletscher |
geographic_facet |
Greenland Petermann Gletscher |
genre |
glacier Greenland Journal of Glaciology North Greenland Petermann gletscher |
genre_facet |
glacier Greenland Journal of Glaciology North Greenland Petermann gletscher |
op_source |
Journal of Glaciology volume 44, issue 148, page 469-476 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000001994 |
container_title |
Journal of Glaciology |
container_volume |
44 |
container_issue |
148 |
container_start_page |
469 |
op_container_end_page |
476 |
_version_ |
1802644480717750272 |