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...
Published in: | Geophysical Research Letters |
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American Geophysical Union
2012
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Online Access: | https://nrl.northumbria.ac.uk/id/eprint/37276/ https://doi.org/10.1029/2012GL051636 |
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ftunivnorthumb:oai:nrl.northumbria.ac.uk:37276 2023-05-15T13:56:54+02:00 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica Makinson, Keith King, Matt Nicholls, Keith Gudmundsson, Hilmar 2012-05-28 https://nrl.northumbria.ac.uk/id/eprint/37276/ https://doi.org/10.1029/2012GL051636 unknown American Geophysical Union Makinson, Keith, King, Matt, Nicholls, Keith and Gudmundsson, Hilmar (2012) Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica. Geophysical Research Letters, 39 (10). L10501. ISSN 0094-8276 F800 Physical and Terrestrial Geographical and Environmental Sciences Article PeerReviewed 2012 ftunivnorthumb https://doi.org/10.1029/2012GL051636 2022-09-25T06:08:49Z 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 Northumbria University, Newcastle: Northumbria Research Link (NRL) 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 |
Northumbria University, Newcastle: Northumbria Research Link (NRL) |
op_collection_id |
ftunivnorthumb |
language |
unknown |
topic |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
spellingShingle |
F800 Physical and Terrestrial Geographical and Environmental Sciences Makinson, Keith King, Matt Nicholls, Keith Gudmundsson, Hilmar Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica |
topic_facet |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
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 Nicholls, Keith Gudmundsson, Hilmar |
author_facet |
Makinson, Keith King, Matt Nicholls, Keith Gudmundsson, 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 |
https://nrl.northumbria.ac.uk/id/eprint/37276/ https://doi.org/10.1029/2012GL051636 |
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 |
Makinson, Keith, King, Matt, Nicholls, Keith and Gudmundsson, Hilmar (2012) Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica. Geophysical Research Letters, 39 (10). L10501. ISSN 0094-8276 |
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 |
_version_ |
1766264500840824832 |