Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry

We present a new technique for mapping the grounding line of Antarctic ice shelves using a combination of CryoSat-2 standard and swath elevation data. Our method is based on detecting the tidal signal in pseudo crossovers, and is tested on the Siple Coast region of West Antarctica. The mapped ground...

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Published in:Geophysical Research Letters
Main Authors: Dawson, Geoffrey, Bamber, Jonathan
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://hdl.handle.net/1983/78750773-9a82-4f38-a87d-2fa2446802cb
https://research-information.bris.ac.uk/en/publications/78750773-9a82-4f38-a87d-2fa2446802cb
https://doi.org/10.1002/2017GL075589
https://research-information.bris.ac.uk/ws/files/139975887/Dawson_et_al_2017_Geophysical_Research_Letters.pdf
id ftubristolcris:oai:research-information.bris.ac.uk:publications/78750773-9a82-4f38-a87d-2fa2446802cb
record_format openpolar
spelling ftubristolcris:oai:research-information.bris.ac.uk:publications/78750773-9a82-4f38-a87d-2fa2446802cb 2024-05-12T07:54:46+00:00 Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry Dawson, Geoffrey Bamber, Jonathan 2017-12-11 application/pdf https://hdl.handle.net/1983/78750773-9a82-4f38-a87d-2fa2446802cb https://research-information.bris.ac.uk/en/publications/78750773-9a82-4f38-a87d-2fa2446802cb https://doi.org/10.1002/2017GL075589 https://research-information.bris.ac.uk/ws/files/139975887/Dawson_et_al_2017_Geophysical_Research_Letters.pdf eng eng https://research-information.bris.ac.uk/en/publications/78750773-9a82-4f38-a87d-2fa2446802cb info:eu-repo/semantics/openAccess Dawson , G & Bamber , J 2017 , ' Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry ' , Geophysical Research Letters . https://doi.org/10.1002/2017GL075589 grounding line CryoSat-2 article 2017 ftubristolcris https://doi.org/10.1002/2017GL075589 2024-04-17T14:26:36Z We present a new technique for mapping the grounding line of Antarctic ice shelves using a combination of CryoSat-2 standard and swath elevation data. Our method is based on detecting the tidal signal in pseudo crossovers, and is tested on the Siple Coast region of West Antarctica. The mapped grounding line is in good agreement with previous observations from differential SAR interferometry (DInSAR) and from ICEsat repeat tracks, with a standard deviation of 1.1 km and 1.0 km, respectively between these methods and ours. There is, however an average seaward bias of 0.6 km, which is due to the poorer precision of CryoSat-2. We have improved coverage particularly near the Echelmeyer Ice Stream where we have shown the grounding zone is approximately 25 km inland from previous estimates. This new method is computationally efficient and can be applied to the rest of Antarctica. Article in Journal/Newspaper Antarc* Antarctic Antarctica Echelmeyer Ice Stream Ice Shelves West Antarctica University of Bristol: Bristol Research Antarctic Echelmeyer Ice Stream ENVELOPE(-150.000,-150.000,-79.167,-79.167) Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Siple Coast ENVELOPE(-155.000,-155.000,-82.000,-82.000) West Antarctica Geophysical Research Letters 44 23 11,886 11,893
institution Open Polar
collection University of Bristol: Bristol Research
op_collection_id ftubristolcris
language English
topic grounding line
CryoSat-2
spellingShingle grounding line
CryoSat-2
Dawson, Geoffrey
Bamber, Jonathan
Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
topic_facet grounding line
CryoSat-2
description We present a new technique for mapping the grounding line of Antarctic ice shelves using a combination of CryoSat-2 standard and swath elevation data. Our method is based on detecting the tidal signal in pseudo crossovers, and is tested on the Siple Coast region of West Antarctica. The mapped grounding line is in good agreement with previous observations from differential SAR interferometry (DInSAR) and from ICEsat repeat tracks, with a standard deviation of 1.1 km and 1.0 km, respectively between these methods and ours. There is, however an average seaward bias of 0.6 km, which is due to the poorer precision of CryoSat-2. We have improved coverage particularly near the Echelmeyer Ice Stream where we have shown the grounding zone is approximately 25 km inland from previous estimates. This new method is computationally efficient and can be applied to the rest of Antarctica.
format Article in Journal/Newspaper
author Dawson, Geoffrey
Bamber, Jonathan
author_facet Dawson, Geoffrey
Bamber, Jonathan
author_sort Dawson, Geoffrey
title Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
title_short Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
title_full Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
title_fullStr Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
title_full_unstemmed Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry
title_sort antarctic grounding line mapping from cryosat-2 radar altimetry
publishDate 2017
url https://hdl.handle.net/1983/78750773-9a82-4f38-a87d-2fa2446802cb
https://research-information.bris.ac.uk/en/publications/78750773-9a82-4f38-a87d-2fa2446802cb
https://doi.org/10.1002/2017GL075589
https://research-information.bris.ac.uk/ws/files/139975887/Dawson_et_al_2017_Geophysical_Research_Letters.pdf
long_lat ENVELOPE(-150.000,-150.000,-79.167,-79.167)
ENVELOPE(-83.917,-83.917,-75.917,-75.917)
ENVELOPE(-155.000,-155.000,-82.000,-82.000)
geographic Antarctic
Echelmeyer Ice Stream
Siple
Siple Coast
West Antarctica
geographic_facet Antarctic
Echelmeyer Ice Stream
Siple
Siple Coast
West Antarctica
genre Antarc*
Antarctic
Antarctica
Echelmeyer Ice Stream
Ice Shelves
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Echelmeyer Ice Stream
Ice Shelves
West Antarctica
op_source Dawson , G & Bamber , J 2017 , ' Antarctic Grounding Line Mapping From CryoSat-2 Radar Altimetry ' , Geophysical Research Letters . https://doi.org/10.1002/2017GL075589
op_relation https://research-information.bris.ac.uk/en/publications/78750773-9a82-4f38-a87d-2fa2446802cb
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1002/2017GL075589
container_title Geophysical Research Letters
container_volume 44
container_issue 23
container_start_page 11,886
op_container_end_page 11,893
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