High-resolution ice-thickness mapping in South Greenland

Airborne radar sounding is difficult in South Greenland because of the presence of englacial water, which prevents the signal from reaching the bed. Data coverage remains suboptimal for traditional methods of ice-thickness and bed mapping that rely on geostatistical techniques, such as kriging, beca...

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Published in:Annals of Glaciology
Main Authors: Morlighem, M, Rignot, E, Mouginot, J, Seroussi, H, Larour, E
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 2014
Subjects:
Online Access:http://www.escholarship.org/uc/item/62s979ms
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spelling ftcdlib:qt62s979ms 2023-05-15T13:29:40+02:00 High-resolution ice-thickness mapping in South Greenland Morlighem, M Rignot, E Mouginot, J Seroussi, H Larour, E 64 - 70 2014-01-01 application/pdf http://www.escholarship.org/uc/item/62s979ms english eng eScholarship, University of California qt62s979ms http://www.escholarship.org/uc/item/62s979ms Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Morlighem, M; Rignot, E; Mouginot, J; Seroussi, H; & Larour, E. (2014). High-resolution ice-thickness mapping in South Greenland. Annals of Glaciology, 55(67), 64 - 70. doi:10.3189/2014AoG67A088. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/62s979ms article 2014 ftcdlib https://doi.org/10.3189/2014AoG67A088 2018-07-13T22:53:56Z Airborne radar sounding is difficult in South Greenland because of the presence of englacial water, which prevents the signal from reaching the bed. Data coverage remains suboptimal for traditional methods of ice-thickness and bed mapping that rely on geostatistical techniques, such as kriging, because important features are missing. Here we apply two alternative approaches of highresolution (̃300 m) ice-thickness mapping, that are based on the conservation of mass, to two regions of South Greenland: (1) Qooqqup Sermia and Kiattuut Sermiat, and (2) Ikertivaq. These two algorithms solve optimization problems, for which the conservation of mass is either enforced as a hard constraint, or as a soft constraint. For the first region, very few measurements are available but there is no gap in ice motion data, whereas for Ikertivaq, more ice-thickness measurements are available, but there are gaps in ice motion data. We show that mass-conservation algorithms can be used as validation tools for radar sounding. We also show that it is preferable to apply mass conservation as a hard constraint, rather than a soft constraint, as it better preserves elongated features, such as glacial valleys and ridges. Article in Journal/Newspaper Annals of Glaciology Greenland University of California: eScholarship Greenland Ikertivaq ENVELOPE(-39.667,-39.667,65.483,65.483) Kiattuut Sermiat ENVELOPE(-45.267,-45.267,61.267,61.267) Annals of Glaciology 55 67 64 70
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language English
description Airborne radar sounding is difficult in South Greenland because of the presence of englacial water, which prevents the signal from reaching the bed. Data coverage remains suboptimal for traditional methods of ice-thickness and bed mapping that rely on geostatistical techniques, such as kriging, because important features are missing. Here we apply two alternative approaches of highresolution (̃300 m) ice-thickness mapping, that are based on the conservation of mass, to two regions of South Greenland: (1) Qooqqup Sermia and Kiattuut Sermiat, and (2) Ikertivaq. These two algorithms solve optimization problems, for which the conservation of mass is either enforced as a hard constraint, or as a soft constraint. For the first region, very few measurements are available but there is no gap in ice motion data, whereas for Ikertivaq, more ice-thickness measurements are available, but there are gaps in ice motion data. We show that mass-conservation algorithms can be used as validation tools for radar sounding. We also show that it is preferable to apply mass conservation as a hard constraint, rather than a soft constraint, as it better preserves elongated features, such as glacial valleys and ridges.
format Article in Journal/Newspaper
author Morlighem, M
Rignot, E
Mouginot, J
Seroussi, H
Larour, E
spellingShingle Morlighem, M
Rignot, E
Mouginot, J
Seroussi, H
Larour, E
High-resolution ice-thickness mapping in South Greenland
author_facet Morlighem, M
Rignot, E
Mouginot, J
Seroussi, H
Larour, E
author_sort Morlighem, M
title High-resolution ice-thickness mapping in South Greenland
title_short High-resolution ice-thickness mapping in South Greenland
title_full High-resolution ice-thickness mapping in South Greenland
title_fullStr High-resolution ice-thickness mapping in South Greenland
title_full_unstemmed High-resolution ice-thickness mapping in South Greenland
title_sort high-resolution ice-thickness mapping in south greenland
publisher eScholarship, University of California
publishDate 2014
url http://www.escholarship.org/uc/item/62s979ms
op_coverage 64 - 70
long_lat ENVELOPE(-39.667,-39.667,65.483,65.483)
ENVELOPE(-45.267,-45.267,61.267,61.267)
geographic Greenland
Ikertivaq
Kiattuut Sermiat
geographic_facet Greenland
Ikertivaq
Kiattuut Sermiat
genre Annals of Glaciology
Greenland
genre_facet Annals of Glaciology
Greenland
op_source Morlighem, M; Rignot, E; Mouginot, J; Seroussi, H; & Larour, E. (2014). High-resolution ice-thickness mapping in South Greenland. Annals of Glaciology, 55(67), 64 - 70. doi:10.3189/2014AoG67A088. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/62s979ms
op_relation qt62s979ms
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op_rights Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.3189/2014AoG67A088
container_title Annals of Glaciology
container_volume 55
container_issue 67
container_start_page 64
op_container_end_page 70
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