Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry
This thesis considers the use of Interferometric Synthetic Aperture Radar (InSAR) for surveying temporal fluctuations in the velocity of glaciers in the Arctic region. The aim of this thesis is to gain a broader understanding of the manner in which the flow of both land- and marine-terminating glaci...
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The University of Edinburgh
2010
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ftunivedinburgh:oai:era.ed.ac.uk:1842/4155 2024-06-09T07:44:05+00:00 Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry Palmer, Steven J. Shepherd, Andrew 2010 application/pdf http://hdl.handle.net/1842/4155 en eng The University of Edinburgh The University of Edinburgh. College of Science and Engineering http://hdl.handle.net/1842/4155 Interferometric Synthetic Aperture Radar InSAR glaciology Greenland Iceland Thesis or Dissertation Doctoral PhD Doctor of Philosophy 2010 ftunivedinburgh 2024-05-10T03:12:17Z This thesis considers the use of Interferometric Synthetic Aperture Radar (InSAR) for surveying temporal fluctuations in the velocity of glaciers in the Arctic region. The aim of this thesis is to gain a broader understanding of the manner in which the flow of both land- and marine-terminating glaciers varies over time, and to asses the ability of InSAR to resolve flow changes over timescales which provide useful information about the physical processes that control them. InSAR makes use of the electromagnetic phase difference between successive SAR images to produce interference patterns (interferograms) which contain information on the topography and motion of the Earth's surface in the direction of the radar line-of-sight. We apply established InSAR techniques (Goldstein et al., 1993) to (i) the 925 km2 LangjÖkull Ice Cap (LIC) in Iceland, which terminates on land (ii) the 8 500 km2 Flade Isblink Icecap (FIIC) in Northeast Greenland which has both land- and marine-terminating glaciers and (iii) to a 7 000 km2 land-terminating sector of the Western Greenland Ice Sheet (GrIS). It is found that these three regions exhibit velocity variations over contrasting timescales. At the LIC, we use an existing ice surface elevation model and dual-look SAR data acquired by the European Remote Sensing (ERS) satellite to estimate ice velocity (Joughin et al., 1998) during late-February in 1994. A comparison with direct velocity measurements determined by global positioning system (GPS) sensors during the summer of 2001 shows agreement (r2 = 0.86), suggesting that the LIC exhibits moderate seasonal and inter-annual variations in ice flow. At the FIIC, we difference pairs of interferograms (Kwok and Fahnestock, 1996) formed using ERS SAR data acquired between 15th August 1995 and 3rd February 1996 to estimate ice velocity on four separate days. We observe that the flow of 5 of the 8 outlet glaciers varies in latesummer compared with winter, although flow speeds vary by up to 20 % over a 10 day period in August 1995. At the ... Doctoral or Postdoctoral Thesis Arctic Greenland Ice cap Ice Sheet Iceland Langjökull Edinburgh Research Archive (ERA - University of Edinburgh) Arctic Greenland Langjökull ENVELOPE(-20.145,-20.145,64.654,64.654) Flade Isblink ENVELOPE(-15.000,-15.000,81.583,81.583) |
institution |
Open Polar |
collection |
Edinburgh Research Archive (ERA - University of Edinburgh) |
op_collection_id |
ftunivedinburgh |
language |
English |
topic |
Interferometric Synthetic Aperture Radar InSAR glaciology Greenland Iceland |
spellingShingle |
Interferometric Synthetic Aperture Radar InSAR glaciology Greenland Iceland Palmer, Steven J. Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
topic_facet |
Interferometric Synthetic Aperture Radar InSAR glaciology Greenland Iceland |
description |
This thesis considers the use of Interferometric Synthetic Aperture Radar (InSAR) for surveying temporal fluctuations in the velocity of glaciers in the Arctic region. The aim of this thesis is to gain a broader understanding of the manner in which the flow of both land- and marine-terminating glaciers varies over time, and to asses the ability of InSAR to resolve flow changes over timescales which provide useful information about the physical processes that control them. InSAR makes use of the electromagnetic phase difference between successive SAR images to produce interference patterns (interferograms) which contain information on the topography and motion of the Earth's surface in the direction of the radar line-of-sight. We apply established InSAR techniques (Goldstein et al., 1993) to (i) the 925 km2 LangjÖkull Ice Cap (LIC) in Iceland, which terminates on land (ii) the 8 500 km2 Flade Isblink Icecap (FIIC) in Northeast Greenland which has both land- and marine-terminating glaciers and (iii) to a 7 000 km2 land-terminating sector of the Western Greenland Ice Sheet (GrIS). It is found that these three regions exhibit velocity variations over contrasting timescales. At the LIC, we use an existing ice surface elevation model and dual-look SAR data acquired by the European Remote Sensing (ERS) satellite to estimate ice velocity (Joughin et al., 1998) during late-February in 1994. A comparison with direct velocity measurements determined by global positioning system (GPS) sensors during the summer of 2001 shows agreement (r2 = 0.86), suggesting that the LIC exhibits moderate seasonal and inter-annual variations in ice flow. At the FIIC, we difference pairs of interferograms (Kwok and Fahnestock, 1996) formed using ERS SAR data acquired between 15th August 1995 and 3rd February 1996 to estimate ice velocity on four separate days. We observe that the flow of 5 of the 8 outlet glaciers varies in latesummer compared with winter, although flow speeds vary by up to 20 % over a 10 day period in August 1995. At the ... |
author2 |
Shepherd, Andrew |
format |
Doctoral or Postdoctoral Thesis |
author |
Palmer, Steven J. |
author_facet |
Palmer, Steven J. |
author_sort |
Palmer, Steven J. |
title |
Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
title_short |
Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
title_full |
Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
title_fullStr |
Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
title_full_unstemmed |
Temporal fluctuations in the motion of Arctic ice masses from satellite radar interferometry |
title_sort |
temporal fluctuations in the motion of arctic ice masses from satellite radar interferometry |
publisher |
The University of Edinburgh |
publishDate |
2010 |
url |
http://hdl.handle.net/1842/4155 |
long_lat |
ENVELOPE(-20.145,-20.145,64.654,64.654) ENVELOPE(-15.000,-15.000,81.583,81.583) |
geographic |
Arctic Greenland Langjökull Flade Isblink |
geographic_facet |
Arctic Greenland Langjökull Flade Isblink |
genre |
Arctic Greenland Ice cap Ice Sheet Iceland Langjökull |
genre_facet |
Arctic Greenland Ice cap Ice Sheet Iceland Langjökull |
op_relation |
The University of Edinburgh. College of Science and Engineering http://hdl.handle.net/1842/4155 |
_version_ |
1801372889608355840 |