Articles | Volume 16, issue 5
https://doi.org/10.5194/cp-16-1999-2020
© Author(s) 2020. 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-16-1999-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Glacial history of Inglefield Land, north Greenland from combined in situ 10Be and 14C exposure dating
Anne Sofie Søndergaard
CORRESPONDING AUTHOR
Department of Geoscience, Aarhus University, Høegh Guldbergs Gade 2, 8000 Aarhus C, Denmark
Nicolaj Krog Larsen
Department of Geoscience, Aarhus University, Høegh Guldbergs Gade 2, 8000 Aarhus C, Denmark
Globe Institute, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark
Olivia Steinemann
Department of Physics, Institute for Particle Physics and
Astrophysics, ETH Zürich, Otto-Stern-Weg 5, 8093 Zürich, Switzerland
Jesper Olsen
Department of Physics and Astronomy, Aarhus University, Ny Munkegade 120, 8000 Aarhus C, Denmark
Svend Funder
Globe Institute, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark
David Lundbek Egholm
Department of Geoscience, Aarhus University, Høegh Guldbergs Gade 2, 8000 Aarhus C, Denmark
Kurt Henrik Kjær
Globe Institute, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark
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Subject: Ice Dynamics | Archive: Terrestrial Archives | Timescale: Holocene
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Marion A. McKenzie, Lauren E. Miller, Allison P. Lepp, and Regina DeWitt
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Records of the interaction between land and glacial ice movement in the Puget Lowland of Washington State are used to interpret that solid Earth movement provided stability to this marine-terminating glacial ice for at least 500 years. These results are significant because this landscape is similar to parts of the Greenland Ice Sheet and the Antarctic Peninsula, indicating that the interactions seen in this area are applicable to modern glaciated regions.
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Short summary
We present new results that show how the north Greenland Ice Sheet responded to climate changes over the last 11 700 years. We find that the ice sheet was very sensitive to past climate changes. Combining our findings with recently published studies reveals distinct differences in sensitivity to past climate changes between northwest and north Greenland. This highlights the sensitivity to past and possible future climate changes of two of the most vulnerable areas of the Greenland Ice Sheet.
We present new results that show how the north Greenland Ice Sheet responded to climate changes...