Greenland-wide accelerated retreat of peripheral glaciers in the twenty-first century
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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1 Online-Ressource.
- Sprache
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Englisch
- Erschienen in
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Greenland-wide accelerated retreat of peripheral glaciers in the twenty-first century ; volume:13 ; number:12 ; day:9 ; month:11 ; year:2023 ; pages:1324-1328 ; date:12.2023
Nature climate change ; 13, Heft 12 (9.11.2023), 1324-1328, 12.2023
- Urheber
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Larocca, L. J.
Twining–Ward, M.
Axford, Y.
Schweinsberg, A. D.
Larsen, S. H.
Westergaard–Nielsen, A.
Luetzenburg, G.
Briner, J. P.
Kjeldsen, K. K.
Bjørk, A. A.
- Beteiligte Personen und Organisationen
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SpringerLink (Online service)
- DOI
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10.1038/s41558-023-01855-6
- URN
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urn:nbn:de:101:1-2024022011452490224180
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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14.08.2025, 10:57 MESZ
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Beteiligte
- Larocca, L. J.
- Twining–Ward, M.
- Axford, Y.
- Schweinsberg, A. D.
- Larsen, S. H.
- Westergaard–Nielsen, A.
- Luetzenburg, G.
- Briner, J. P.
- Kjeldsen, K. K.
- Bjørk, A. A.
- SpringerLink (Online service)
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Centennial response of Greenland’s three largest outlet glaciers
Can katabatic winds directly force retreat of Greenland outlet glaciers? Hypothesis test on Helheim Glacier in Sermilik Fjord
Younger Dryas ice-margin retreat in Greenland, new evidence from Southwest Greenland
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Sediment discharge from Greenland’s marine-terminating glaciers is linked with surface melt
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Submarine melting of glaciers in Greenland amplified by atmospheric warming
Multi-decadal retreat of marine-terminating outlet glaciers in northwest and central-west Greenland
Multi-decadal retreat of marine-terminating outlet glaciers in northwest and central-west Greenland
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Younger Dryas ice margin retreat in Greenland: new evidence from southwestern Greenland
Accelerating retreat and high-elevation thinning of glaciers in central Spitsbergen
Sediment discharge from Greenland’s marine-terminating glaciers is linked with surface melt
Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica
Comparison of four calving laws to model Greenland outlet glaciers
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