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 tongue of Petermann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automat-ically from differential inte...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.612.807 2023-05-15T16:21:04+02:00 Hinge‐line migration of Petermann Gletscher, north Greenland, detected using satellite‐radar interferometry Eric Rignot The Pennsylvania State University CiteSeerX Archives 1998 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.807 http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.807 http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf text 1998 ftciteseerx 2016-01-08T14:35:41Z 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 tongue of Petermann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automat-ically 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 multi-date image data to a precision of 5 m, 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 f 7 0 m, 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 f120 m. The retreat suggests glacier thinning at a rate of 7 8 f 3 5 cm ice awl. Coincidentally, an analysis of ice volume fluxes indicates that the hinge line ice flux of Petermann Gletscher exceeds its balance flux by 0. 8 8 f l krn3icea-', which in turn implies glacier thinning at 8 3 f 9 5 cm ice a- ' in the glacier lower reaches. Both methods therefore suggest that Petermann Gletscher is currently losing mass to the ocean. 1 Text glacier Greenland North Greenland Petermann gletscher Unknown Awl ENVELOPE(-60.633,-60.633,-63.867,-63.867) Greenland Petermann Gletscher ENVELOPE(-59.500,-59.500,80.500,80.500) |
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Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
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 tongue of Petermann Gletscher, a major outlet glacier of north Greenland. The hinge line is detected automat-ically 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 multi-date image data to a precision of 5 m, 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 f 7 0 m, 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 f120 m. The retreat suggests glacier thinning at a rate of 7 8 f 3 5 cm ice awl. Coincidentally, an analysis of ice volume fluxes indicates that the hinge line ice flux of Petermann Gletscher exceeds its balance flux by 0. 8 8 f l krn3icea-', which in turn implies glacier thinning at 8 3 f 9 5 cm ice a- ' in the glacier lower reaches. Both methods therefore suggest that Petermann Gletscher is currently losing mass to the ocean. 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Eric Rignot |
spellingShingle |
Eric Rignot Hinge‐line migration of Petermann Gletscher, north Greenland, detected using satellite‐radar interferometry |
author_facet |
Eric Rignot |
author_sort |
Eric Rignot |
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 |
publishDate |
1998 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.807 http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf |
long_lat |
ENVELOPE(-60.633,-60.633,-63.867,-63.867) ENVELOPE(-59.500,-59.500,80.500,80.500) |
geographic |
Awl Greenland Petermann Gletscher |
geographic_facet |
Awl Greenland Petermann Gletscher |
genre |
glacier Greenland North Greenland Petermann gletscher |
genre_facet |
glacier Greenland North Greenland Petermann gletscher |
op_source |
http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.807 http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/19518/1/98-0936.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766009080896290816 |