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WeightNameValue
1000 Titel
  • Assessing the potential for ice flow piracy between the Totten and Vanderford glaciers, East Antarctica
1000 Autor/in
  1. McCormack, Felicity S. |
  2. Roberts, Jason L. |
  3. Kulessa, Bernd |
  4. Aitken, Alan |
  5. Dow, Christine F. |
  6. Bird, Lawrence |
  7. Galton-Fenzi, Benjamin K. |
  8. Hochmuth, Katharina |
  9. Jones, Richard S. |
  10. Mackintosh, Andrew N. |
  11. McArthur, Koi |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2023
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2023-11-01
1000 Erschienen in
1000 Quellenangabe
  • 17(11):4549-4569
1000 Copyrightjahr
  • 2023
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-17-4549-2023 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The largest regional drivers of current surface elevation increases in the Antarctic Ice Sheet are associated with ice flow reconfiguration in previously active ice streams, highlighting the important role of ice dynamics in mass balance calculations. Here, we investigate controls on the evolution of the flow configuration of the Vanderford and Totten glaciers – key outlet glaciers of the Aurora Subglacial Basin (ASB) – the most rapidly thinning region of the East Antarctic Ice Sheet (EAIS). We synthesise factors that influence the ice flow in this region and use an ice sheet model to investigate the sensitivity of the catchment divide location to changes in surface elevation due to thinning at the Vanderford Glacier (VG) associated with ongoing retreat and thickening at the Totten Glacier (TG) associated with an intensification of the east–west snowfall gradient. The present-day catchment divide between the Totten and Vanderford glaciers is not constrained by the geology or topography but is determined by the large-scale ice sheet geometry and its long-term evolution in response to climate forcing. Furthermore, the catchment divide migrates under relatively small changes in surface elevation, leading to ice flow and basal water piracy from the Totten to the Vanderford Glacier. Our findings show that ice flow reconfigurations occur not only in regions of West Antarctica like the Siple Coast but also in the east, motivating further investigations of past, and the potential for future, ice flow reconfigurations around the whole Antarctic coastline. Modelling of ice flow and basal water piracy may require coupled ice sheet thermomechanical and subglacial hydrology models constrained by field observations of subglacial conditions. Our results have implications for ice sheet mass budget studies that integrate over catchments and the validity of the zero flow assumption when selecting sites for ice core records of past climate. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/TWNDb3JtYWNrLCBGZWxpY2l0ecKgUy4=|https://frl.publisso.de/adhoc/uri/Um9iZXJ0cywgSmFzb27CoEwu|https://frl.publisso.de/adhoc/uri/S3VsZXNzYSwgQmVybmQ=|https://frl.publisso.de/adhoc/uri/QWl0a2VuLCBBbGFu|https://frl.publisso.de/adhoc/uri/RG93LCBDaHJpc3RpbmXCoEYu|https://frl.publisso.de/adhoc/uri/QmlyZCwgTGF3cmVuY2U=|https://frl.publisso.de/adhoc/uri/R2FsdG9uLUZlbnppLCBCZW5qYW1pbsKgSy4=|https://frl.publisso.de/adhoc/uri/SG9jaG11dGgsIEthdGhhcmluYQ==|https://frl.publisso.de/adhoc/uri/Sm9uZXMsIFJpY2hhcmTCoFMu|https://frl.publisso.de/adhoc/uri/TWFja2ludG9zaCwgQW5kcmV3wqBOLg==|https://frl.publisso.de/adhoc/uri/TWNBcnRodXIsIEtvaQ==
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  1. Australian Research Council |
  2. Natural Sciences and Engineering Research Council of Canada |
  3. Canada Research Chairs |
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1000 Dateien
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1000 Erstellt am 2024-05-21T20:28:57.279+0200
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