A method of calculating ice-shelf surface velocity using ICESat altimetry
ABSTRACT Very high precision satellite altimeter measurements from the Geoscience Laser Altimeter System onboard NASA's Ice, Cloud and Land Elevation Satellite (ICESat) have allowed a method of feature tracking to be developed for floating ice which relies on recording the movement of large sur...
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Online Access: | http://dx.doi.org/10.1017/s0032247411000362 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247411000362 |
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crcambridgeupr:10.1017/s0032247411000362 2024-03-03T08:38:39+00:00 A method of calculating ice-shelf surface velocity using ICESat altimetry Marsh, O.J. Rack, W. 2011 http://dx.doi.org/10.1017/s0032247411000362 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247411000362 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 48, issue 1, page 25-30 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 2011 crcambridgeupr https://doi.org/10.1017/s0032247411000362 2024-02-08T08:33:10Z ABSTRACT Very high precision satellite altimeter measurements from the Geoscience Laser Altimeter System onboard NASA's Ice, Cloud and Land Elevation Satellite (ICESat) have allowed a method of feature tracking to be developed for floating ice which relies on recording the movement of large surface undulations. This method is applied to a section of the Ross Ice Shelf downstream of the grounding line of the Beardmore Glacier, Antarctica. The altimetry method has benefits over established optical and interferometric remote sensing techniques due to high pointing accuracy for geo-location, ability to deal with tidal fluctuations and to measure velocity where visible surface features are absent. Initial processing of a single sequence of ICESat tracks gives encouraging results for unidirectional ice flow with correlations between surface profiles in consecutive years exceeding 90% and producing high internal consistency in velocity between independent tracks. Velocities of 331 ± 28 m a −1 near to the grounding line are also consistent with available ground measurements for the area. Article in Journal/Newspaper Antarc* Antarctica Beardmore Glacier Ice Shelf Polar Record Ross Ice Shelf Cambridge University Press Ross Ice Shelf Beardmore ENVELOPE(174.900,174.900,-83.350,-83.350) Beardmore Glacier ENVELOPE(170.000,170.000,-84.500,-84.500) Polar Record 48 1 25 30 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development Marsh, O.J. Rack, W. A method of calculating ice-shelf surface velocity using ICESat altimetry |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
description |
ABSTRACT Very high precision satellite altimeter measurements from the Geoscience Laser Altimeter System onboard NASA's Ice, Cloud and Land Elevation Satellite (ICESat) have allowed a method of feature tracking to be developed for floating ice which relies on recording the movement of large surface undulations. This method is applied to a section of the Ross Ice Shelf downstream of the grounding line of the Beardmore Glacier, Antarctica. The altimetry method has benefits over established optical and interferometric remote sensing techniques due to high pointing accuracy for geo-location, ability to deal with tidal fluctuations and to measure velocity where visible surface features are absent. Initial processing of a single sequence of ICESat tracks gives encouraging results for unidirectional ice flow with correlations between surface profiles in consecutive years exceeding 90% and producing high internal consistency in velocity between independent tracks. Velocities of 331 ± 28 m a −1 near to the grounding line are also consistent with available ground measurements for the area. |
format |
Article in Journal/Newspaper |
author |
Marsh, O.J. Rack, W. |
author_facet |
Marsh, O.J. Rack, W. |
author_sort |
Marsh, O.J. |
title |
A method of calculating ice-shelf surface velocity using ICESat altimetry |
title_short |
A method of calculating ice-shelf surface velocity using ICESat altimetry |
title_full |
A method of calculating ice-shelf surface velocity using ICESat altimetry |
title_fullStr |
A method of calculating ice-shelf surface velocity using ICESat altimetry |
title_full_unstemmed |
A method of calculating ice-shelf surface velocity using ICESat altimetry |
title_sort |
method of calculating ice-shelf surface velocity using icesat altimetry |
publisher |
Cambridge University Press (CUP) |
publishDate |
2011 |
url |
http://dx.doi.org/10.1017/s0032247411000362 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247411000362 |
long_lat |
ENVELOPE(174.900,174.900,-83.350,-83.350) ENVELOPE(170.000,170.000,-84.500,-84.500) |
geographic |
Ross Ice Shelf Beardmore Beardmore Glacier |
geographic_facet |
Ross Ice Shelf Beardmore Beardmore Glacier |
genre |
Antarc* Antarctica Beardmore Glacier Ice Shelf Polar Record Ross Ice Shelf |
genre_facet |
Antarc* Antarctica Beardmore Glacier Ice Shelf Polar Record Ross Ice Shelf |
op_source |
Polar Record volume 48, issue 1, page 25-30 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247411000362 |
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Polar Record |
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48 |
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1 |
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25 |
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30 |
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1792507072746618880 |