Effects of Waves on Tabular Ice-Shelf Calving
As a conveyor belt transferring inland ice to ocean, ice shelves shed mass through large, systematic tabular calving, which also plays a major role in the fluctuation of the buttressing forces. Tabular iceberg calving involves two stages: first is systematic cracking, which develops after the forwar...
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American Geophysical Union
2014
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Online Access: | https://hdl.handle.net/20.500.11937/33318 https://doi.org/10.1175/EI-D-14-0005.1 |
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ftcurtin:oai:espace.curtin.edu.au:20.500.11937/33318 2023-06-11T04:04:00+02:00 Effects of Waves on Tabular Ice-Shelf Calving Ren, Diandong Leslie, Lance 2014 restricted https://hdl.handle.net/20.500.11937/33318 https://doi.org/10.1175/EI-D-14-0005.1 unknown American Geophysical Union http://hdl.handle.net/20.500.11937/33318 doi:10.1175/EI-D-14-0005.1 Ice-sheet–ocean interaction Surface mass balance Climate change Antarctic Ice Sheet Ice-shelf calving Tabular ice-shelf attrition Journal Article 2014 ftcurtin https://doi.org/20.500.11937/3331810.1175/EI-D-14-0005.1 2023-05-30T19:37:34Z As a conveyor belt transferring inland ice to ocean, ice shelves shed mass through large, systematic tabular calving, which also plays a major role in the fluctuation of the buttressing forces. Tabular iceberg calving involves two stages: first is systematic cracking, which develops after the forward-slanting front reaches a limiting extension length determined by gravity–buoyancy imbalance; second is fatigue separation. The latter has greater variability, producing calving irregularity. Whereas ice flow vertical shear determines the timing of the systematic cracking, wave actions are decisive for ensuing viscoplastic fatigue. Because the frontal section has its own resonance frequency, it reverberates only to waves of similar frequency. With a flow-dependent, nonlocal attrition scheme, the present ice model [Scalable Extensible Geoflow Model for Environmental Research-Ice flow submodel (SEGMENT-Ice)] describes an entire ice-shelf life cycle.It is found that most East Antarctic ice shelves have higher resonance frequencies, and the fatigue of viscoplastic ice is significantly enhanced by shoaling waves from both storm surges and infragravity waves (~5 × 10−3 Hz). The two largest embayed ice shelves have resonance frequencies within the range of tsunami waves. When approaching critical extension lengths, perturbations from about four consecutive tsunami events can cause complete separation of tabular icebergs from shelves. For shelves with resonance frequencies matching storm surge waves, future reduction of sea ice may impose much larger deflections from shoaling, storm-generated ocean waves. Although the Ross Ice Shelf (RIS) total mass varies little in the twenty-first century, the mass turnover quickens and the ice conveyor belt is ~40% more efficient by the late twenty-first century, reaching 70 km3 yr−1. The mass distribution shifts oceanward, favoring future tabular calving. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Iceberg* Ross Ice Shelf Sea ice Curtin University: espace Antarctic Ross Ice Shelf Earth Interactions 18 13 1 28 |
institution |
Open Polar |
collection |
Curtin University: espace |
op_collection_id |
ftcurtin |
language |
unknown |
topic |
Ice-sheet–ocean interaction Surface mass balance Climate change Antarctic Ice Sheet Ice-shelf calving Tabular ice-shelf attrition |
spellingShingle |
Ice-sheet–ocean interaction Surface mass balance Climate change Antarctic Ice Sheet Ice-shelf calving Tabular ice-shelf attrition Ren, Diandong Leslie, Lance Effects of Waves on Tabular Ice-Shelf Calving |
topic_facet |
Ice-sheet–ocean interaction Surface mass balance Climate change Antarctic Ice Sheet Ice-shelf calving Tabular ice-shelf attrition |
description |
As a conveyor belt transferring inland ice to ocean, ice shelves shed mass through large, systematic tabular calving, which also plays a major role in the fluctuation of the buttressing forces. Tabular iceberg calving involves two stages: first is systematic cracking, which develops after the forward-slanting front reaches a limiting extension length determined by gravity–buoyancy imbalance; second is fatigue separation. The latter has greater variability, producing calving irregularity. Whereas ice flow vertical shear determines the timing of the systematic cracking, wave actions are decisive for ensuing viscoplastic fatigue. Because the frontal section has its own resonance frequency, it reverberates only to waves of similar frequency. With a flow-dependent, nonlocal attrition scheme, the present ice model [Scalable Extensible Geoflow Model for Environmental Research-Ice flow submodel (SEGMENT-Ice)] describes an entire ice-shelf life cycle.It is found that most East Antarctic ice shelves have higher resonance frequencies, and the fatigue of viscoplastic ice is significantly enhanced by shoaling waves from both storm surges and infragravity waves (~5 × 10−3 Hz). The two largest embayed ice shelves have resonance frequencies within the range of tsunami waves. When approaching critical extension lengths, perturbations from about four consecutive tsunami events can cause complete separation of tabular icebergs from shelves. For shelves with resonance frequencies matching storm surge waves, future reduction of sea ice may impose much larger deflections from shoaling, storm-generated ocean waves. Although the Ross Ice Shelf (RIS) total mass varies little in the twenty-first century, the mass turnover quickens and the ice conveyor belt is ~40% more efficient by the late twenty-first century, reaching 70 km3 yr−1. The mass distribution shifts oceanward, favoring future tabular calving. |
format |
Article in Journal/Newspaper |
author |
Ren, Diandong Leslie, Lance |
author_facet |
Ren, Diandong Leslie, Lance |
author_sort |
Ren, Diandong |
title |
Effects of Waves on Tabular Ice-Shelf Calving |
title_short |
Effects of Waves on Tabular Ice-Shelf Calving |
title_full |
Effects of Waves on Tabular Ice-Shelf Calving |
title_fullStr |
Effects of Waves on Tabular Ice-Shelf Calving |
title_full_unstemmed |
Effects of Waves on Tabular Ice-Shelf Calving |
title_sort |
effects of waves on tabular ice-shelf calving |
publisher |
American Geophysical Union |
publishDate |
2014 |
url |
https://hdl.handle.net/20.500.11937/33318 https://doi.org/10.1175/EI-D-14-0005.1 |
geographic |
Antarctic Ross Ice Shelf |
geographic_facet |
Antarctic Ross Ice Shelf |
genre |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Iceberg* Ross Ice Shelf Sea ice |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Iceberg* Ross Ice Shelf Sea ice |
op_relation |
http://hdl.handle.net/20.500.11937/33318 doi:10.1175/EI-D-14-0005.1 |
op_doi |
https://doi.org/20.500.11937/3331810.1175/EI-D-14-0005.1 |
container_title |
Earth Interactions |
container_volume |
18 |
container_issue |
13 |
container_start_page |
1 |
op_container_end_page |
28 |
_version_ |
1768384900049666048 |