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, Nicholls, Keith, Gudmundsson, Hilmar
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2012
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/37276/
https://doi.org/10.1029/2012GL051636
id ftunivnorthumb:oai:nrl.northumbria.ac.uk:37276
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spelling 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
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