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1000 Titel
  • The effect of landfast sea ice buttressing on ice dynamic speedup in the Larsen B embayment, Antarctica
1000 Autor/in
  1. Surawy-Stepney, Trystan |
  2. Hogg, Anna E. |
  3. Cornford, Stephen L. |
  4. Wallis, Benjamin J. |
  5. Davison, Benjamin J. |
  6. Selley, Heather L. |
  7. Slater, Ross A. W. |
  8. Lie, Elise K. |
  9. Jakob, Livia |
  10. Ridout, Andrew |
  11. Gourmelen, Noel |
  12. Freer, Bryony I. D. |
  13. Wilson, Sally F. |
  14. Shepherd, Andrew |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-03-04
1000 Erschienen in
1000 Quellenangabe
  • 18(3):977-993
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-977-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. We observe the evacuation of 11-year-old landfast sea ice in the Larsen B embayment on the East Antarctic Peninsula in January 2022, which was in part triggered by warm atmospheric conditions and strong offshore winds. This evacuation of sea ice was closely followed by major changes in the calving behaviour and dynamics of a subset of the ocean-terminating glaciers in the region. We show using satellite measurements that, following a decade of gradual slow-down, Hektoria, Green, and Crane glaciers sped up by approximately 20 %–50 % between February and the end of 2022, each increasing in speed by more than 100 m a−1. Circumstantially, this is attributable to their transition into tidewater glaciers following the loss of their ice shelves after the landfast sea ice evacuation. However, a question remains as to whether the landfast sea ice could have influenced the dynamics of these glaciers, or the stability of their ice shelves, through a buttressing effect akin to that of confined ice shelves on grounded ice streams. We show, with a series of diagnostic modelling experiments, that direct landfast sea ice buttressing had a negligible impact on the dynamics of the grounded ice streams. Furthermore, we suggest that the loss of landfast sea ice buttressing could have impacted the dynamics of the rheologically weak ice shelves, in turn diminishing their stability over time; however, the accompanying shifts in the distributions of resistive stress within the ice shelves would have been minor. This indicates that this loss of buttressing by landfast sea ice is likely to have been a secondary process in the ice shelf disaggregation compared to, for example, increased ocean swell or the drivers of the initial landfast sea ice disintegration. </jats:p>
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  2. Natural Environment Research Council |
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1000 Dateien
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    1000 Förderer European Space Agency |
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    1000 Förderer Natural Environment Research Council |
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1000 Erstellt am 2024-05-23T13:52:23.469+0200
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1000 Zuletzt bearbeitet Mon May 27 11:21:41 CEST 2024
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