Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica

Recent GPS observations from a spatially extensive network across Ronne Ice Shelf show significant daily ice flow variations. At all sites, the almost-synchronous horizontal displacements occur at diurnal and semidiurnal tidal periods. During spring tides, displacements, velocities and strains near...

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Published in:Geophysical Research Letters
Main Authors: Makinson, Keith, King, Matt A., Nicholls, Keith W., Gudmundsson, G. Hilmar
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2012
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/18612/
https://nora.nerc.ac.uk/id/eprint/18612/1/grl29179.pdf
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spelling ftnerc:oai:nora.nerc.ac.uk:18612 2023-05-15T13:45:12+02:00 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica Makinson, Keith King, Matt A. Nicholls, Keith W. Gudmundsson, G. Hilmar 2012 text http://nora.nerc.ac.uk/id/eprint/18612/ https://nora.nerc.ac.uk/id/eprint/18612/1/grl29179.pdf en eng American Geophysical Union https://nora.nerc.ac.uk/id/eprint/18612/1/grl29179.pdf Makinson, Keith orcid:0000-0002-5791-1767 King, Matt A.; Nicholls, Keith W. orcid:0000-0002-2188-4509 Gudmundsson, G. Hilmar orcid:0000-0003-4236-5369 . 2012 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica. Geophysical Research Letters, 39, L10501. 5, pp. https://doi.org/10.1029/2012GL051636 <https://doi.org/10.1029/2012GL051636> Publication - Article PeerReviewed 2012 ftnerc https://doi.org/10.1029/2012GL051636 2023-02-04T19:31:51Z Recent GPS observations from a spatially extensive network across Ronne Ice Shelf show significant daily ice flow variations. At all sites, the almost-synchronous horizontal displacements occur at diurnal and semidiurnal tidal periods. During spring tides, displacements, velocities and strains near the ice front have superimposed oscillations that are ±300% of their mean values and occur over a six-hour period, resulting in regular ice shelf flow reversals. Close to ice stream grounding lines, however, the horizontal diurnal and semidiurnal signals decay and almost vanish. From our analysis, we conclude that ice shelves respond primarily elastically to tidal tilting, thus accounting for the observed diurnal and semidiurnal flow variations, and their amplification toward the ice shelf front. Our findings suggest that detailed modeling of these data could provide improved ice shelf and ice stream models for correctly simulating ice shelf flow and predicting future ice sheet evolution Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf Ice Shelves Ronne Ice Shelf Natural Environment Research Council: NERC Open Research Archive Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500) Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) Geophysical Research Letters 39 10 n/a n/a
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description Recent GPS observations from a spatially extensive network across Ronne Ice Shelf show significant daily ice flow variations. At all sites, the almost-synchronous horizontal displacements occur at diurnal and semidiurnal tidal periods. During spring tides, displacements, velocities and strains near the ice front have superimposed oscillations that are ±300% of their mean values and occur over a six-hour period, resulting in regular ice shelf flow reversals. Close to ice stream grounding lines, however, the horizontal diurnal and semidiurnal signals decay and almost vanish. From our analysis, we conclude that ice shelves respond primarily elastically to tidal tilting, thus accounting for the observed diurnal and semidiurnal flow variations, and their amplification toward the ice shelf front. Our findings suggest that detailed modeling of these data could provide improved ice shelf and ice stream models for correctly simulating ice shelf flow and predicting future ice sheet evolution
format Article in Journal/Newspaper
author Makinson, Keith
King, Matt A.
Nicholls, Keith W.
Gudmundsson, G. Hilmar
spellingShingle Makinson, Keith
King, Matt A.
Nicholls, Keith W.
Gudmundsson, G. Hilmar
Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
author_facet Makinson, Keith
King, Matt A.
Nicholls, Keith W.
Gudmundsson, G. Hilmar
author_sort Makinson, Keith
title Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_short Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_full Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_fullStr Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_full_unstemmed Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_sort diurnal and semidiurnal tide-induced lateral movement of ronne ice shelf, antarctica
publisher American Geophysical Union
publishDate 2012
url http://nora.nerc.ac.uk/id/eprint/18612/
https://nora.nerc.ac.uk/id/eprint/18612/1/grl29179.pdf
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
ENVELOPE(-54.065,-54.065,49.700,49.700)
geographic Ronne Ice Shelf
Tilting
geographic_facet Ronne Ice Shelf
Tilting
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
op_relation https://nora.nerc.ac.uk/id/eprint/18612/1/grl29179.pdf
Makinson, Keith orcid:0000-0002-5791-1767
King, Matt A.; Nicholls, Keith W. orcid:0000-0002-2188-4509
Gudmundsson, G. Hilmar orcid:0000-0003-4236-5369 . 2012 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica. Geophysical Research Letters, 39, L10501. 5, pp. https://doi.org/10.1029/2012GL051636 <https://doi.org/10.1029/2012GL051636>
op_doi https://doi.org/10.1029/2012GL051636
container_title Geophysical Research Letters
container_volume 39
container_issue 10
container_start_page n/a
op_container_end_page n/a
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