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...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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2012
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Online Access: | https://figshare.com/articles/journal_contribution/Diurnal_and_semidiurnal_tide-induced_lateral_movement_of_Ronne_Ice_Shelf_Antarctica/22908719 |
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author | Makinson, K Matt King Nicholls, KW Gudmundsson, GH |
author_facet | Makinson, K Matt King Nicholls, KW Gudmundsson, GH |
author_sort | Makinson, K |
collection | Research from University Of Tasmania |
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 |
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 |
geographic | Ronne Ice Shelf Tilting |
geographic_facet | Ronne Ice Shelf Tilting |
id | ftunivtasmanfig:oai:figshare.com:article/22908719 |
institution | Open Polar |
language | unknown |
long_lat | ENVELOPE(-61.000,-61.000,-78.500,-78.500) ENVELOPE(-54.065,-54.065,49.700,49.700) |
op_collection_id | ftunivtasmanfig |
op_relation | 102.100.100/577572 |
op_rights | In Copyright |
publishDate | 2012 |
record_format | openpolar |
spelling | ftunivtasmanfig:oai:figshare.com:article/22908719 2025-03-16T15:18:01+00:00 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica Makinson, K Matt King Nicholls, KW Gudmundsson, GH 2012-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/Diurnal_and_semidiurnal_tide-induced_lateral_movement_of_Ronne_Ice_Shelf_Antarctica/22908719 unknown 102.100.100/577572 In Copyright Geodesy Antarctica ice sheets tides Text Journal contribution 2012 ftunivtasmanfig 2025-02-17T09:48:20Z 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 Research from University Of Tasmania Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500) Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) |
spellingShingle | Geodesy Antarctica ice sheets tides Makinson, K Matt King Nicholls, KW Gudmundsson, GH Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica |
title | 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_short | 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 |
topic | Geodesy Antarctica ice sheets tides |
topic_facet | Geodesy Antarctica ice sheets tides |
url | https://figshare.com/articles/journal_contribution/Diurnal_and_semidiurnal_tide-induced_lateral_movement_of_Ronne_Ice_Shelf_Antarctica/22908719 |