Articles | Volume 17, issue 2
https://doi.org/10.5194/cp-17-587-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-587-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Mar 2021
Research article |
| 04 Mar 2021
| 04 Mar 2021
Younger Dryas ice margin retreat in Greenland: new evidence from southwestern Greenland
Svend Funder
CORRESPONDING AUTHOR
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
Anita H. L. Sørensen
Geosyd, 2730 Copenhagen, Denmark
Nicolaj K. Larsen
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
Anders A. Bjørk
Department of Geoscience and Natural Resource Management, University of
Copenhagen, 1350 Copenhagen, Denmark
Jason P. Briner
Department of Geology, University at Buffalo, Buffalo, NY 14260, USA
Jesper Olsen
Department of Physics and Astronomy, Aarhus University, 8000 Aarhus,
Denmark
Anders Schomacker
Department of Geosciences, UiT, the Arctic University of Norway, 9037
Tromsø, Norway
Laura B. Levy
Department of Geology, Humboldt State University, 1 Harpst St. Arcata, CA
95521, USA
Kurt H. Kjær
Globe Institute, University of Copenhagen, 1350 Copenhagen, Denmark
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Cited
12 citations as recorded by crossref.
- Abrupt warming and alpine glacial retreat through the last deglaciation in Alaska interrupted by modest Northern Hemisphere cooling J. Tulenko et al. 10.5194/cp-20-625-2024
- Marine conditions and development of the Sirius Water polynya on the North-East Greenland shelf during the Younger Dryas-Holocene R. Jackson et al. 10.1016/j.quascirev.2022.107647
- A High Arctic inner shelf–fjord system from the Last Glacial Maximum to the present: Bessel Fjord and southwest Dove Bugt, northeastern Greenland K. Zoller et al. 10.5194/cp-19-1321-2023
- The Northeast Pacific Ocean and Northwest Coast of North America within the global climate system, 29,000 to 11,700 years ago D. Mann & B. Gaglioti 10.1016/j.earscirev.2024.104782
- From land to sea: provenance, composition, and preservation of organic matter in a marine sediment record from the North‐East Greenland shelf spanning the Younger Dryas–Holocene N. Andreasen et al. 10.1111/bor.12630
- Last deglacial abrupt climate changes caused by meltwater pulses in the Labrador Sea D. You et al. 10.1038/s43247-023-00743-3
- Heinrich summers G. Denton et al. 10.1016/j.quascirev.2022.107750
- Direct evidence for thinning and retreat of the southernmost Greenland ice sheet during the Younger Dryas A. Carlson et al. 10.1016/j.quascirev.2021.107105
- Retreat patterns and dynamics of the former Norske Trough ice stream (NE Greenland): An integrated geomorphological and sedimentological approach A. López-Quirós et al. 10.1016/j.quascirev.2023.108477
- Late glacial and Holocene glaciation history of North and Northeast Greenland N. Larsen et al. 10.1080/15230430.2022.2094607
- Late Quaternary changes in sediment sources in the Labrador Sea J. Andrews & D. Piper 10.1139/cjes-2022-0026
- Lateglacial Shifts in Seasonality Reconcile Conflicting North Atlantic Temperature Signals G. Bromley et al. 10.1029/2022JF006951
12 citations as recorded by crossref.
- Abrupt warming and alpine glacial retreat through the last deglaciation in Alaska interrupted by modest Northern Hemisphere cooling J. Tulenko et al. 10.5194/cp-20-625-2024
- Marine conditions and development of the Sirius Water polynya on the North-East Greenland shelf during the Younger Dryas-Holocene R. Jackson et al. 10.1016/j.quascirev.2022.107647
- A High Arctic inner shelf–fjord system from the Last Glacial Maximum to the present: Bessel Fjord and southwest Dove Bugt, northeastern Greenland K. Zoller et al. 10.5194/cp-19-1321-2023
- The Northeast Pacific Ocean and Northwest Coast of North America within the global climate system, 29,000 to 11,700 years ago D. Mann & B. Gaglioti 10.1016/j.earscirev.2024.104782
- From land to sea: provenance, composition, and preservation of organic matter in a marine sediment record from the North‐East Greenland shelf spanning the Younger Dryas–Holocene N. Andreasen et al. 10.1111/bor.12630
- Last deglacial abrupt climate changes caused by meltwater pulses in the Labrador Sea D. You et al. 10.1038/s43247-023-00743-3
- Heinrich summers G. Denton et al. 10.1016/j.quascirev.2022.107750
- Direct evidence for thinning and retreat of the southernmost Greenland ice sheet during the Younger Dryas A. Carlson et al. 10.1016/j.quascirev.2021.107105
- Retreat patterns and dynamics of the former Norske Trough ice stream (NE Greenland): An integrated geomorphological and sedimentological approach A. López-Quirós et al. 10.1016/j.quascirev.2023.108477
- Late glacial and Holocene glaciation history of North and Northeast Greenland N. Larsen et al. 10.1080/15230430.2022.2094607
- Late Quaternary changes in sediment sources in the Labrador Sea J. Andrews & D. Piper 10.1139/cjes-2022-0026
- Lateglacial Shifts in Seasonality Reconcile Conflicting North Atlantic Temperature Signals G. Bromley et al. 10.1029/2022JF006951
Latest update: 17 Nov 2024
Short summary
Cosmogenic 10Be exposure dates from outlying islets along 300 km of the SW Greenland coast indicate that, although affected by inherited 10Be, the ice margin here was retreating during the Younger Dryas. These results seem to be corroborated by recent studies elsewhere in Greenland. The apparent mismatch between temperatures and ice margin behaviour may be explained by the advection of warm water to the ice margin on the shelf and by increased seasonality, both caused by a weakened AMOC.
Cosmogenic 10Be exposure dates from outlying islets along 300 km of the SW Greenland coast...
