Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes

We analyze data acquired by the CryoSat-2 interferometric radar altimeter and demonstrate its novel capability to track topographic features on the Antarctic Ice Sheet. We map the perimeter and depth of a 260 km2 surface depression above an Antarctic subglacial lake (SGL) and, in combination with Ic...

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Published in:Geophysical Research Letters
Main Authors: McMillan, Malcolm, Corr, Hugh, Shepherd, Andrew, Ridout, Andrew, Laxon, Seymour, Cullen, Robert
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
Subjects:
Online Access:https://eprints.lancs.ac.uk/id/eprint/128844/
https://doi.org/10.1002/grl.50689
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spelling ftulancaster:oai:eprints.lancs.ac.uk:128844 2023-08-27T04:06:15+02:00 Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes McMillan, Malcolm Corr, Hugh Shepherd, Andrew Ridout, Andrew Laxon, Seymour Cullen, Robert 2013-08-28 https://eprints.lancs.ac.uk/id/eprint/128844/ https://doi.org/10.1002/grl.50689 unknown McMillan, Malcolm and Corr, Hugh and Shepherd, Andrew and Ridout, Andrew and Laxon, Seymour and Cullen, Robert (2013) Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes. Geophysical Research Letters, 40 (16). pp. 4321-4327. ISSN 0094-8276 Journal Article PeerReviewed 2013 ftulancaster https://doi.org/10.1002/grl.50689 2023-08-03T22:34:21Z We analyze data acquired by the CryoSat-2 interferometric radar altimeter and demonstrate its novel capability to track topographic features on the Antarctic Ice Sheet. We map the perimeter and depth of a 260 km2 surface depression above an Antarctic subglacial lake (SGL) and, in combination with Ice, Cloud and land Elevation Satellite laser altimetry, chart decadal changes in SGL volume. During 2007-2008, between 4.9 and 6.4 km3 of water drained from the SGL, and peak discharge exceeded 160 m3 s -1. The flood was twice as large as any previously recorded and equivalent to ~ 10% of the meltwater generated annually beneath the ice sheet. The ice surface has since uplifted at a rate of 5.6 ± 2.8 m yr -1. Our study demonstrates the ability of CryoSat-2 to provide detailed maps of ice sheet topography, its potential to accurately measure SGL drainage events, and the contribution it can make to understanding water flow beneath Antarctica. Key Points Assessment of novel CryoSat-2 interferometric altimetry over land ice Demonstration of interferometric capability to track off-nadir topography Mapping of largest Antarctic subglacial lake drainage event observed to date. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Lancaster University: Lancaster Eprints Antarctic The Antarctic Geophysical Research Letters 40 16 4321 4327
institution Open Polar
collection Lancaster University: Lancaster Eprints
op_collection_id ftulancaster
language unknown
description We analyze data acquired by the CryoSat-2 interferometric radar altimeter and demonstrate its novel capability to track topographic features on the Antarctic Ice Sheet. We map the perimeter and depth of a 260 km2 surface depression above an Antarctic subglacial lake (SGL) and, in combination with Ice, Cloud and land Elevation Satellite laser altimetry, chart decadal changes in SGL volume. During 2007-2008, between 4.9 and 6.4 km3 of water drained from the SGL, and peak discharge exceeded 160 m3 s -1. The flood was twice as large as any previously recorded and equivalent to ~ 10% of the meltwater generated annually beneath the ice sheet. The ice surface has since uplifted at a rate of 5.6 ± 2.8 m yr -1. Our study demonstrates the ability of CryoSat-2 to provide detailed maps of ice sheet topography, its potential to accurately measure SGL drainage events, and the contribution it can make to understanding water flow beneath Antarctica. Key Points Assessment of novel CryoSat-2 interferometric altimetry over land ice Demonstration of interferometric capability to track off-nadir topography Mapping of largest Antarctic subglacial lake drainage event observed to date.
format Article in Journal/Newspaper
author McMillan, Malcolm
Corr, Hugh
Shepherd, Andrew
Ridout, Andrew
Laxon, Seymour
Cullen, Robert
spellingShingle McMillan, Malcolm
Corr, Hugh
Shepherd, Andrew
Ridout, Andrew
Laxon, Seymour
Cullen, Robert
Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
author_facet McMillan, Malcolm
Corr, Hugh
Shepherd, Andrew
Ridout, Andrew
Laxon, Seymour
Cullen, Robert
author_sort McMillan, Malcolm
title Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
title_short Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
title_full Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
title_fullStr Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
title_full_unstemmed Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes
title_sort three-dimensional mapping by cryosat-2 of subglacial lake volume changes
publishDate 2013
url https://eprints.lancs.ac.uk/id/eprint/128844/
https://doi.org/10.1002/grl.50689
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_relation McMillan, Malcolm and Corr, Hugh and Shepherd, Andrew and Ridout, Andrew and Laxon, Seymour and Cullen, Robert (2013) Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes. Geophysical Research Letters, 40 (16). pp. 4321-4327. ISSN 0094-8276
op_doi https://doi.org/10.1002/grl.50689
container_title Geophysical Research Letters
container_volume 40
container_issue 16
container_start_page 4321
op_container_end_page 4327
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