Rapid ice discharge from southeast Greenland glaciers
Interferometric synthetic-aperture radar (InSAR) observations of southeast Greenland glaciers acquired by the Earth Remote Sensing Satellites (ERS-1/2) in 1996 were combined with ice sounding radar data collected in the late 1990s to estimate a total discharge of 46 ± 3 km 3 ice per year between 62°...
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Language: | English |
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ftcdlib:qt7528r5pw 2023-05-15T16:03:47+02:00 Rapid ice discharge from southeast Greenland glaciers Rignot, E Braaten, D Gogineni, SP Krabill, WB McConnell, JR L10401 1-4 2004-05-28 application/pdf http://www.escholarship.org/uc/item/7528r5pw english eng eScholarship, University of California qt7528r5pw http://www.escholarship.org/uc/item/7528r5pw Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Rignot, E; Braaten, D; Gogineni, SP; Krabill, WB; & McConnell, JR. (2004). Rapid ice discharge from southeast Greenland glaciers. Geophysical Research Letters, 31(10), L10401 1-4. doi:10.1029/2004GL019474. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/7528r5pw article 2004 ftcdlib https://doi.org/10.1029/2004GL019474 2018-07-06T22:51:32Z Interferometric synthetic-aperture radar (InSAR) observations of southeast Greenland glaciers acquired by the Earth Remote Sensing Satellites (ERS-1/2) in 1996 were combined with ice sounding radar data collected in the late 1990s to estimate a total discharge of 46 ± 3 km 3 ice per year between 62°N and 66°N, which is significantly lower than a mass input of 29 ± 3 km 3 ice per year calculated from a recent compilation of snow accumulation data. Further north, Helheim Glacier discharges 23 ± 1 km 3/yr vs 30 ± 3 km 3/yr accumulation; Kangerdlugssuaq Glacier discharges 29 ± 2 km 3/yr vs 23 ± km 3/yr; and Daugaard-Jensen Glacier discharges 10.5 ± 0.6 km 3/yr vs 10.5 ± 1 km 3/yr. The mass balance of east Greenland glaciers is therefore dominated by the negative mass balance of southeast Greenland glaciers (- 17 ± 4 km 3/yr), equivalent to a sea level rise of 0.04 ± 0.01 mm/yr. Warmer and drier conditions cannot explain the imbalance which we attribute to longterm changes in ice dynamics. Copyright 2004 by the American Geophysical Union. Article in Journal/Newspaper East Greenland glacier Greenland University of California: eScholarship Greenland Jensen Glacier ENVELOPE(170.800,170.800,-85.083,-85.083) Geophysical Research Letters 31 10 n/a n/a |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
English |
description |
Interferometric synthetic-aperture radar (InSAR) observations of southeast Greenland glaciers acquired by the Earth Remote Sensing Satellites (ERS-1/2) in 1996 were combined with ice sounding radar data collected in the late 1990s to estimate a total discharge of 46 ± 3 km 3 ice per year between 62°N and 66°N, which is significantly lower than a mass input of 29 ± 3 km 3 ice per year calculated from a recent compilation of snow accumulation data. Further north, Helheim Glacier discharges 23 ± 1 km 3/yr vs 30 ± 3 km 3/yr accumulation; Kangerdlugssuaq Glacier discharges 29 ± 2 km 3/yr vs 23 ± km 3/yr; and Daugaard-Jensen Glacier discharges 10.5 ± 0.6 km 3/yr vs 10.5 ± 1 km 3/yr. The mass balance of east Greenland glaciers is therefore dominated by the negative mass balance of southeast Greenland glaciers (- 17 ± 4 km 3/yr), equivalent to a sea level rise of 0.04 ± 0.01 mm/yr. Warmer and drier conditions cannot explain the imbalance which we attribute to longterm changes in ice dynamics. Copyright 2004 by the American Geophysical Union. |
format |
Article in Journal/Newspaper |
author |
Rignot, E Braaten, D Gogineni, SP Krabill, WB McConnell, JR |
spellingShingle |
Rignot, E Braaten, D Gogineni, SP Krabill, WB McConnell, JR Rapid ice discharge from southeast Greenland glaciers |
author_facet |
Rignot, E Braaten, D Gogineni, SP Krabill, WB McConnell, JR |
author_sort |
Rignot, E |
title |
Rapid ice discharge from southeast Greenland glaciers |
title_short |
Rapid ice discharge from southeast Greenland glaciers |
title_full |
Rapid ice discharge from southeast Greenland glaciers |
title_fullStr |
Rapid ice discharge from southeast Greenland glaciers |
title_full_unstemmed |
Rapid ice discharge from southeast Greenland glaciers |
title_sort |
rapid ice discharge from southeast greenland glaciers |
publisher |
eScholarship, University of California |
publishDate |
2004 |
url |
http://www.escholarship.org/uc/item/7528r5pw |
op_coverage |
L10401 1-4 |
long_lat |
ENVELOPE(170.800,170.800,-85.083,-85.083) |
geographic |
Greenland Jensen Glacier |
geographic_facet |
Greenland Jensen Glacier |
genre |
East Greenland glacier Greenland |
genre_facet |
East Greenland glacier Greenland |
op_source |
Rignot, E; Braaten, D; Gogineni, SP; Krabill, WB; & McConnell, JR. (2004). Rapid ice discharge from southeast Greenland glaciers. Geophysical Research Letters, 31(10), L10401 1-4. doi:10.1029/2004GL019474. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/7528r5pw |
op_relation |
qt7528r5pw http://www.escholarship.org/uc/item/7528r5pw |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/2004GL019474 |
container_title |
Geophysical Research Letters |
container_volume |
31 |
container_issue |
10 |
container_start_page |
n/a |
op_container_end_page |
n/a |
_version_ |
1766399469664862208 |