Extensive and anomalous grounding line retreat at Vanderford Glacier, Vincennes Bay, Wilkes Land, East Antarctica
Abstract - 1, places Vanderford Glacier as the fastest retreating glacier in East Antarctica, and the third fastest in Antarctica, across decadal timescales. Such rapid retreat is consistent with the hypothesis that warm mCDW is able to access deep cavities formed below the Vanderford Ice Shelf, driving high rates of basal melting close to the grounding line. With a retrograde slope observed inland along the Vanderford Trench, such oceanic forcing may have significant implications for the future stability of Vanderford Glacier.
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Erschienen in
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Extensive and anomalous grounding line retreat at Vanderford Glacier, Vincennes Bay, Wilkes Land, East Antarctica ; volume:17 ; number:8 ; year:2023 ; pages:3593-3616 ; extent:24
The Cryosphere ; 17, Heft 8 (2023), 3593-3616 (gesamt 24)
- Urheber
- DOI
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10.5194/tc-17-3593-2023
- URN
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urn:nbn:de:101:1-2023083104275753350457
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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14.08.2025, 11:00 MESZ
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Beteiligte
- Picton, Hannah J.
- Stokes, Chris R.
- Jamieson, Stewart S. R.
- Floricioiu, Dana
- Krieger, Lukas
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Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea
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Basal channels, ice thinning and grounding zone retreat at Thwaites Glacier, West Antarctica
Grounding line retreat and tide-modulated ocean channels at Moscow University and Totten Glacier ice shelves, East Antarctica
Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica
Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
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Ongoing grounding line retreat and fracturation initiated at the Petermann Glacier ice shelf, Greenland after 2016
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