Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones
Differential interferometric synthetic aperture radar (DInSAR) is an essential tool for detecting ice-sheet motion near Antarctica's oceanic margin. These space-borne measurements have been used extensively in the past to map the location and retreat of ice-shelf grounding lines as an indicator...
Published in: | The Cryosphere |
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Language: | English |
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Copernicus Publications on behalf of the European Geosciences Union
2019
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Online Access: | http://nora.nerc.ac.uk/id/eprint/526102/ https://nora.nerc.ac.uk/id/eprint/526102/1/tc-13-3171-2019.pdf https://doi.org/10.5194/tc-13-3171-2019 |
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ftnerc:oai:nora.nerc.ac.uk:526102 2023-05-15T13:41:44+02:00 Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones Wild, Christian T. Marsh, Oliver J. Rack, Wolfgang 2019-11-29 text http://nora.nerc.ac.uk/id/eprint/526102/ https://nora.nerc.ac.uk/id/eprint/526102/1/tc-13-3171-2019.pdf https://doi.org/10.5194/tc-13-3171-2019 en eng Copernicus Publications on behalf of the European Geosciences Union https://nora.nerc.ac.uk/id/eprint/526102/1/tc-13-3171-2019.pdf Wild, Christian T.; Marsh, Oliver J. orcid:0000-0001-7874-514X Rack, Wolfgang. 2019 Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones. The Cryosphere, 13 (12). 3171-3191. https://doi.org/10.5194/tc-13-3171-2019 <https://doi.org/10.5194/tc-13-3171-2019> cc_by_4 CC-BY Publication - Article PeerReviewed 2019 ftnerc https://doi.org/10.5194/tc-13-3171-2019 2023-02-04T19:49:47Z Differential interferometric synthetic aperture radar (DInSAR) is an essential tool for detecting ice-sheet motion near Antarctica's oceanic margin. These space-borne measurements have been used extensively in the past to map the location and retreat of ice-shelf grounding lines as an indicator for the onset of marine ice-sheet instability and to calculate the mass balance of ice sheets and individual catchments. The main difficulty in interpreting DInSAR is that images originate from a combination of several SAR images and do not indicate instantaneous ice deflection at the times of satellite data acquisitions. Here, we combine the sub-centimetre accuracy and spatial benefits of DInSAR with the temporal benefits of tide models to infer the spatio-temporal dynamics of ice–ocean interaction during the times of satellite overpasses. We demonstrate the potential of this synergy with TerraSAR-X data from the almost-stagnant southern McMurdo Ice Shelf (SMIS). We then validate our algorithm with GPS data from the fast-flowing Darwin Glacier, draining the Antarctic Plateau through the Transantarctic Mountains into the Ross Sea. We are able to reconstruct DInSAR-derived vertical displacements to 7 mm mean absolute residual error and generally improve traditional tide-model output by up to 39 % from 10.8 to 6.7 cm RMSE against GPS data from areas where ice is in local hydrostatic equilibrium with the ocean and by up to 74 % from 21.4 to 5.6 cm RMSE against GPS data in feature-rich coastal areas where tide models have not been applicable before. Numerical modelling then reveals Young's modulus of E=1.0±0.56 GPa and an ice viscosity of ν=10±3.65 TPa s when finite-element simulations of tidal flexure are matched to 16 d of tiltmeter data, supporting the hypothesis that strain-dependent anisotropy may significantly decrease effective viscosity compared to isotropic polycrystalline ice on large spatial scales. Applications of our method include the following: refining coarsely gridded tide models to resolve small-scale ... Article in Journal/Newspaper Antarc* Antarctic Darwin Glacier Ice Sheet Ice Shelf McMurdo Ice Shelf Ross Sea The Cryosphere Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Ross Sea Transantarctic Mountains McMurdo Ice Shelf ENVELOPE(166.500,166.500,-78.000,-78.000) Darwin Glacier ENVELOPE(159.000,159.000,-79.883,-79.883) The Cryosphere 13 12 3171 3191 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
Differential interferometric synthetic aperture radar (DInSAR) is an essential tool for detecting ice-sheet motion near Antarctica's oceanic margin. These space-borne measurements have been used extensively in the past to map the location and retreat of ice-shelf grounding lines as an indicator for the onset of marine ice-sheet instability and to calculate the mass balance of ice sheets and individual catchments. The main difficulty in interpreting DInSAR is that images originate from a combination of several SAR images and do not indicate instantaneous ice deflection at the times of satellite data acquisitions. Here, we combine the sub-centimetre accuracy and spatial benefits of DInSAR with the temporal benefits of tide models to infer the spatio-temporal dynamics of ice–ocean interaction during the times of satellite overpasses. We demonstrate the potential of this synergy with TerraSAR-X data from the almost-stagnant southern McMurdo Ice Shelf (SMIS). We then validate our algorithm with GPS data from the fast-flowing Darwin Glacier, draining the Antarctic Plateau through the Transantarctic Mountains into the Ross Sea. We are able to reconstruct DInSAR-derived vertical displacements to 7 mm mean absolute residual error and generally improve traditional tide-model output by up to 39 % from 10.8 to 6.7 cm RMSE against GPS data from areas where ice is in local hydrostatic equilibrium with the ocean and by up to 74 % from 21.4 to 5.6 cm RMSE against GPS data in feature-rich coastal areas where tide models have not been applicable before. Numerical modelling then reveals Young's modulus of E=1.0±0.56 GPa and an ice viscosity of ν=10±3.65 TPa s when finite-element simulations of tidal flexure are matched to 16 d of tiltmeter data, supporting the hypothesis that strain-dependent anisotropy may significantly decrease effective viscosity compared to isotropic polycrystalline ice on large spatial scales. Applications of our method include the following: refining coarsely gridded tide models to resolve small-scale ... |
format |
Article in Journal/Newspaper |
author |
Wild, Christian T. Marsh, Oliver J. Rack, Wolfgang |
spellingShingle |
Wild, Christian T. Marsh, Oliver J. Rack, Wolfgang Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
author_facet |
Wild, Christian T. Marsh, Oliver J. Rack, Wolfgang |
author_sort |
Wild, Christian T. |
title |
Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
title_short |
Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
title_full |
Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
title_fullStr |
Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
title_full_unstemmed |
Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones |
title_sort |
differential interferometric synthetic aperture radar for tide modelling in antarctic ice-shelf grounding zones |
publisher |
Copernicus Publications on behalf of the European Geosciences Union |
publishDate |
2019 |
url |
http://nora.nerc.ac.uk/id/eprint/526102/ https://nora.nerc.ac.uk/id/eprint/526102/1/tc-13-3171-2019.pdf https://doi.org/10.5194/tc-13-3171-2019 |
long_lat |
ENVELOPE(166.500,166.500,-78.000,-78.000) ENVELOPE(159.000,159.000,-79.883,-79.883) |
geographic |
Antarctic The Antarctic Ross Sea Transantarctic Mountains McMurdo Ice Shelf Darwin Glacier |
geographic_facet |
Antarctic The Antarctic Ross Sea Transantarctic Mountains McMurdo Ice Shelf Darwin Glacier |
genre |
Antarc* Antarctic Darwin Glacier Ice Sheet Ice Shelf McMurdo Ice Shelf Ross Sea The Cryosphere |
genre_facet |
Antarc* Antarctic Darwin Glacier Ice Sheet Ice Shelf McMurdo Ice Shelf Ross Sea The Cryosphere |
op_relation |
https://nora.nerc.ac.uk/id/eprint/526102/1/tc-13-3171-2019.pdf Wild, Christian T.; Marsh, Oliver J. orcid:0000-0001-7874-514X Rack, Wolfgang. 2019 Differential interferometric synthetic aperture radar for tide modelling in Antarctic ice-shelf grounding zones. The Cryosphere, 13 (12). 3171-3191. https://doi.org/10.5194/tc-13-3171-2019 <https://doi.org/10.5194/tc-13-3171-2019> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/tc-13-3171-2019 |
container_title |
The Cryosphere |
container_volume |
13 |
container_issue |
12 |
container_start_page |
3171 |
op_container_end_page |
3191 |
_version_ |
1766156297548333056 |