Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland

We infer the horizontal velocity fields of the ice caps Langjökull and Hofsjökull, central Iceland, using repeat-pass interferometric synthetic aperture radar (InSAR). NASA's uninhabited aerial vehicle synthetic aperture radar (UAVSAR) acquired airborne InSAR data from multiple vantage points...

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Published in:Journal of Glaciology
Main Authors: Minchew, Brent, Simons, Mark, Hensley, Scott, Björnsson, Helgi, Pálsson, Finnur
Format: Article in Journal/Newspaper
Language:unknown
Published: Cambridge University Press 2015
Subjects:
Online Access:https://doi.org/10.3189/2015JoG14J023
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spelling ftcaltechauth:oai:authors.library.caltech.edu:ev1ez-n2a56 2024-10-13T14:07:27+00:00 Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland Minchew, Brent Simons, Mark Hensley, Scott Björnsson, Helgi Pálsson, Finnur 2015 https://doi.org/10.3189/2015JoG14J023 unknown Cambridge University Press https://doi.org/10.3189/2015JoG14J023 eprintid:87671 info:eu-repo/semantics/openAccess Other Journal of Glaciology, 61(226), 253-266, (2015) glacier flow glaciological instruments and methods ice cap ice velocity remote sensing info:eu-repo/semantics/article 2015 ftcaltechauth https://doi.org/10.3189/2015JoG14J023 2024-09-25T18:46:37Z We infer the horizontal velocity fields of the ice caps Langjökull and Hofsjökull, central Iceland, using repeat-pass interferometric synthetic aperture radar (InSAR). NASA's uninhabited aerial vehicle synthetic aperture radar (UAVSAR) acquired airborne InSAR data from multiple vantage points during the early melt season in June 2012. We develop a Bayesian approach for inferring three-dimensional velocity fields from multiple InSAR acquisitions. The horizontal components generally agree with available GPS measurements wherever ice motion is well constrained by InSAR observations. We provide evidence that changes in volumetric moisture content near the glacier surface induce phase offsets that obfuscate the vertical component of the surface velocity fields, an effect that could manifest itself on any glacier that experiences surface melt. Spatial patterns in the InSAR-derived horizontal speeds are broadly consistent with the results of a simple viscous flow model, and the directionality of the InSAR-derived horizontal flow field is nearly everywhere consistent with the ice surface gradient. Significant differences between the InSAR-derived horizontal speed and the speed predicted by the viscous flow model suggest that basal slip accounts for more than half the observed outlet glacier flow. © 2015 International Glaciological Society. MS received 25 January 2014 and accepted in revised form 30 November 2014. Published online: 10 July 2017. Funding for the UAVSAR campaign was provided by NASA's Cryospheric Sciences Program. B.M. was supported by a NASA Earth and Space Sciences fellowship and an ARCS Foundation fellowship. We thank the UAVSAR team and the NASA-Dryden flight crew who collected and helped process the InSAR data, T. Jóhannesson for providing the Hofsjökull surface DEM, S. Owen for assistance with GIPSY-OASIS and F. Ortega for reviewing the manuscript. Published - early_melt_season_velocity_fields_of_langjokull_and_hofsjokull_central_iceland.pdf Article in Journal/Newspaper glacier Ice cap Iceland Journal of Glaciology Caltech Authors (California Institute of Technology) Ortega ENVELOPE(-57.950,-57.950,-63.950,-63.950) Journal of Glaciology 61 226 253 266
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic glacier flow
glaciological instruments and methods
ice cap
ice velocity
remote sensing
spellingShingle glacier flow
glaciological instruments and methods
ice cap
ice velocity
remote sensing
Minchew, Brent
Simons, Mark
Hensley, Scott
Björnsson, Helgi
Pálsson, Finnur
Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
topic_facet glacier flow
glaciological instruments and methods
ice cap
ice velocity
remote sensing
description We infer the horizontal velocity fields of the ice caps Langjökull and Hofsjökull, central Iceland, using repeat-pass interferometric synthetic aperture radar (InSAR). NASA's uninhabited aerial vehicle synthetic aperture radar (UAVSAR) acquired airborne InSAR data from multiple vantage points during the early melt season in June 2012. We develop a Bayesian approach for inferring three-dimensional velocity fields from multiple InSAR acquisitions. The horizontal components generally agree with available GPS measurements wherever ice motion is well constrained by InSAR observations. We provide evidence that changes in volumetric moisture content near the glacier surface induce phase offsets that obfuscate the vertical component of the surface velocity fields, an effect that could manifest itself on any glacier that experiences surface melt. Spatial patterns in the InSAR-derived horizontal speeds are broadly consistent with the results of a simple viscous flow model, and the directionality of the InSAR-derived horizontal flow field is nearly everywhere consistent with the ice surface gradient. Significant differences between the InSAR-derived horizontal speed and the speed predicted by the viscous flow model suggest that basal slip accounts for more than half the observed outlet glacier flow. © 2015 International Glaciological Society. MS received 25 January 2014 and accepted in revised form 30 November 2014. Published online: 10 July 2017. Funding for the UAVSAR campaign was provided by NASA's Cryospheric Sciences Program. B.M. was supported by a NASA Earth and Space Sciences fellowship and an ARCS Foundation fellowship. We thank the UAVSAR team and the NASA-Dryden flight crew who collected and helped process the InSAR data, T. Jóhannesson for providing the Hofsjökull surface DEM, S. Owen for assistance with GIPSY-OASIS and F. Ortega for reviewing the manuscript. Published - early_melt_season_velocity_fields_of_langjokull_and_hofsjokull_central_iceland.pdf
format Article in Journal/Newspaper
author Minchew, Brent
Simons, Mark
Hensley, Scott
Björnsson, Helgi
Pálsson, Finnur
author_facet Minchew, Brent
Simons, Mark
Hensley, Scott
Björnsson, Helgi
Pálsson, Finnur
author_sort Minchew, Brent
title Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
title_short Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
title_full Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
title_fullStr Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
title_full_unstemmed Early melt season velocity fields of Langjökull and Hofsjökull, central Iceland
title_sort early melt season velocity fields of langjã¶kull and hofsjã¶kull, central iceland
publisher Cambridge University Press
publishDate 2015
url https://doi.org/10.3189/2015JoG14J023
long_lat ENVELOPE(-57.950,-57.950,-63.950,-63.950)
geographic Ortega
geographic_facet Ortega
genre glacier
Ice cap
Iceland
Journal of Glaciology
genre_facet glacier
Ice cap
Iceland
Journal of Glaciology
op_source Journal of Glaciology, 61(226), 253-266, (2015)
op_relation https://doi.org/10.3189/2015JoG14J023
eprintid:87671
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.3189/2015JoG14J023
container_title Journal of Glaciology
container_volume 61
container_issue 226
container_start_page 253
op_container_end_page 266
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