Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry

We employ a time series of Sentinel-1 differential radar interferometry data from year 2018 to detect the variability of the grounding line position of the Fisher, Mellor and Lambert glaciers, which drain an ice volume equivalent to an 8-m sea level rise from East Antarctica. We observe kilometer-sc...

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Main Authors: Chen, Hanning, Rignot, Eric, Scheuchl, Bernd, Ehrenfeucht, Shivani
Format: Dataset
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/7564225
https://doi.org/10.7280/D1FT44
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:7564225 2023-05-15T13:22:07+02:00 Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry Chen, Hanning Rignot, Eric Scheuchl, Bernd Ehrenfeucht, Shivani 2023-01-23 https://zenodo.org/record/7564225 https://doi.org/10.7280/D1FT44 unknown https://zenodo.org/communities/dryad https://zenodo.org/record/7564225 https://doi.org/10.7280/D1FT44 oai:zenodo.org:7564225 info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/legalcode info:eu-repo/semantics/other dataset 2023 ftzenodo https://doi.org/10.7280/D1FT44 2023-03-10T22:08:13Z We employ a time series of Sentinel-1 differential radar interferometry data from year 2018 to detect the variability of the grounding line position of the Fisher, Mellor and Lambert glaciers, which drain an ice volume equivalent to an 8-m sea level rise from East Antarctica. We observe kilometer-scale tidal migration, two orders of magnitude larger than expected for ice in hydrostatic equilibrium on a hard bed. The migration is not in phase with changes in oceanic tide. In two major estuaries underlaid by subglacial channels, we observe two states of migration that switch on and off over time scales of several weeks. The range of vertical motion indicates a water column thickness of 2 to 20 centimeters. Such intrusions over wide grounding zones are not accounted for in physical models. Including wide grounding zone with vigorous melt will enhance the sensitivity of glaciers to ocean warming and increase the projections of mass loss. Funding provided by: University of California, IrvineCrossref Funder Registry ID: http://dx.doi.org/10.13039/100008476Award Number: Dataset Amery Ice Shelf Antarc* Antarctica East Antarctica Ice Shelf Zenodo East Antarctica Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) Mellor ENVELOPE(-114.944,-114.944,60.714,60.714)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description We employ a time series of Sentinel-1 differential radar interferometry data from year 2018 to detect the variability of the grounding line position of the Fisher, Mellor and Lambert glaciers, which drain an ice volume equivalent to an 8-m sea level rise from East Antarctica. We observe kilometer-scale tidal migration, two orders of magnitude larger than expected for ice in hydrostatic equilibrium on a hard bed. The migration is not in phase with changes in oceanic tide. In two major estuaries underlaid by subglacial channels, we observe two states of migration that switch on and off over time scales of several weeks. The range of vertical motion indicates a water column thickness of 2 to 20 centimeters. Such intrusions over wide grounding zones are not accounted for in physical models. Including wide grounding zone with vigorous melt will enhance the sensitivity of glaciers to ocean warming and increase the projections of mass loss. Funding provided by: University of California, IrvineCrossref Funder Registry ID: http://dx.doi.org/10.13039/100008476Award Number:
format Dataset
author Chen, Hanning
Rignot, Eric
Scheuchl, Bernd
Ehrenfeucht, Shivani
spellingShingle Chen, Hanning
Rignot, Eric
Scheuchl, Bernd
Ehrenfeucht, Shivani
Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
author_facet Chen, Hanning
Rignot, Eric
Scheuchl, Bernd
Ehrenfeucht, Shivani
author_sort Chen, Hanning
title Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
title_short Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
title_full Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
title_fullStr Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
title_full_unstemmed Data for: Grounding zone of Amery Ice Shelf, Antarctica, from differential synthetic-aperture radar interferometry
title_sort data for: grounding zone of amery ice shelf, antarctica, from differential synthetic-aperture radar interferometry
publishDate 2023
url https://zenodo.org/record/7564225
https://doi.org/10.7280/D1FT44
long_lat ENVELOPE(-94.063,-94.063,56.565,56.565)
ENVELOPE(71.000,71.000,-69.750,-69.750)
ENVELOPE(-114.944,-114.944,60.714,60.714)
geographic East Antarctica
Amery
Amery Ice Shelf
Mellor
geographic_facet East Antarctica
Amery
Amery Ice Shelf
Mellor
genre Amery Ice Shelf
Antarc*
Antarctica
East Antarctica
Ice Shelf
genre_facet Amery Ice Shelf
Antarc*
Antarctica
East Antarctica
Ice Shelf
op_relation https://zenodo.org/communities/dryad
https://zenodo.org/record/7564225
https://doi.org/10.7280/D1FT44
oai:zenodo.org:7564225
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.7280/D1FT44
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