Antarctic Ice Sheet grounding line discharge from 1996 through 2023

Grounding line discharge is a key component of the mass balance of the Antarctic Ice Sheet. Here we present an estimate of Antarctic Ice Sheet grounding line discharge from 1996 through to last month. We calculate ice flux at up to 100 m resolution through 16 algorithmically-generated flux gates, wh...

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Main Authors: Davison, Benjamin Joseph, Hogg, Anna Elizabeth, Slater, Thomas, Rigby, Richard
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/essd-2023-448
https://essd.copernicus.org/preprints/essd-2023-448/
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spelling ftcopernicus:oai:publications.copernicus.org:essdd115697 2023-12-24T10:09:20+01:00 Antarctic Ice Sheet grounding line discharge from 1996 through 2023 Davison, Benjamin Joseph Hogg, Anna Elizabeth Slater, Thomas Rigby, Richard 2023-11-24 application/pdf https://doi.org/10.5194/essd-2023-448 https://essd.copernicus.org/preprints/essd-2023-448/ eng eng doi:10.5194/essd-2023-448 https://essd.copernicus.org/preprints/essd-2023-448/ eISSN: 1866-3516 Text 2023 ftcopernicus https://doi.org/10.5194/essd-2023-448 2023-11-27T17:24:17Z Grounding line discharge is a key component of the mass balance of the Antarctic Ice Sheet. Here we present an estimate of Antarctic Ice Sheet grounding line discharge from 1996 through to last month. We calculate ice flux at up to 100 m resolution through 16 algorithmically-generated flux gates, which are continuous around Antarctica. We draw on a range of ice velocity and thickness data to estimate grounding line discharge. For ice thickness, we use four bed topography datasets, two firn models and a temporally varying ice surface. For the ice velocity, we utilise a range of publicly-available ice velocity maps at resolutions ranging from 240 x 240 m to 1000 x 1000 m, as well as new, 100 x 100 m monthly velocity mosaics derived from intensity-tracking of Sentinel-1 image pairs, available since October 2014. The pixel-based ice fluxes and ice flux errors are integrated within all available Antarctic ice stream, ice shelf and glacier basins. Our dataset also includes the contributions to discharge from changes in ice thickness due to surface lowering, time-varying firn air content and surface mass change between the flux gates and grounding line. We find that Antarctic Ice Sheet grounding line discharge increased from 1,990 ± 23 Gt yr -1 to 2,205 ± 18 Gt yr -1 between 1996 and 2023, much of which was due to acceleration of ice streams in West Antarctica but with substantial contributions from ice streams in East Antarctica and glaciers on the Antarctic Peninsula. The uncertainties in our discharge dataset primarily result from uncertain bed elevation and flux gate location, which account for much of difference between our results and previous studies. It is our intention to update this discharge dataset each month, subject to continued Sentinel-1 acquisitions and funding availability. The datasets are freely available at https://zenodo.org/records/10183327 (Davison et al., 2023a). Text Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica Ice Sheet Ice Shelf West Antarctica Copernicus Publications: E-Journals Antarctic The Antarctic Antarctic Peninsula East Antarctica West Antarctica
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Grounding line discharge is a key component of the mass balance of the Antarctic Ice Sheet. Here we present an estimate of Antarctic Ice Sheet grounding line discharge from 1996 through to last month. We calculate ice flux at up to 100 m resolution through 16 algorithmically-generated flux gates, which are continuous around Antarctica. We draw on a range of ice velocity and thickness data to estimate grounding line discharge. For ice thickness, we use four bed topography datasets, two firn models and a temporally varying ice surface. For the ice velocity, we utilise a range of publicly-available ice velocity maps at resolutions ranging from 240 x 240 m to 1000 x 1000 m, as well as new, 100 x 100 m monthly velocity mosaics derived from intensity-tracking of Sentinel-1 image pairs, available since October 2014. The pixel-based ice fluxes and ice flux errors are integrated within all available Antarctic ice stream, ice shelf and glacier basins. Our dataset also includes the contributions to discharge from changes in ice thickness due to surface lowering, time-varying firn air content and surface mass change between the flux gates and grounding line. We find that Antarctic Ice Sheet grounding line discharge increased from 1,990 ± 23 Gt yr -1 to 2,205 ± 18 Gt yr -1 between 1996 and 2023, much of which was due to acceleration of ice streams in West Antarctica but with substantial contributions from ice streams in East Antarctica and glaciers on the Antarctic Peninsula. The uncertainties in our discharge dataset primarily result from uncertain bed elevation and flux gate location, which account for much of difference between our results and previous studies. It is our intention to update this discharge dataset each month, subject to continued Sentinel-1 acquisitions and funding availability. The datasets are freely available at https://zenodo.org/records/10183327 (Davison et al., 2023a).
format Text
author Davison, Benjamin Joseph
Hogg, Anna Elizabeth
Slater, Thomas
Rigby, Richard
spellingShingle Davison, Benjamin Joseph
Hogg, Anna Elizabeth
Slater, Thomas
Rigby, Richard
Antarctic Ice Sheet grounding line discharge from 1996 through 2023
author_facet Davison, Benjamin Joseph
Hogg, Anna Elizabeth
Slater, Thomas
Rigby, Richard
author_sort Davison, Benjamin Joseph
title Antarctic Ice Sheet grounding line discharge from 1996 through 2023
title_short Antarctic Ice Sheet grounding line discharge from 1996 through 2023
title_full Antarctic Ice Sheet grounding line discharge from 1996 through 2023
title_fullStr Antarctic Ice Sheet grounding line discharge from 1996 through 2023
title_full_unstemmed Antarctic Ice Sheet grounding line discharge from 1996 through 2023
title_sort antarctic ice sheet grounding line discharge from 1996 through 2023
publishDate 2023
url https://doi.org/10.5194/essd-2023-448
https://essd.copernicus.org/preprints/essd-2023-448/
geographic Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
West Antarctica
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
West Antarctica
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
West Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
West Antarctica
op_source eISSN: 1866-3516
op_relation doi:10.5194/essd-2023-448
https://essd.copernicus.org/preprints/essd-2023-448/
op_doi https://doi.org/10.5194/essd-2023-448
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