Communications Earth & Environment (Nov 2022)
Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning Maud Land, East Antarctica
- Yusuke Suganuma,
- Heitaro Kaneda,
- Martim Mas e Braga,
- Takeshige Ishiwa,
- Takushi Koyama,
- Jennifer C. Newall,
- Jun’ichi Okuno,
- Takashi Obase,
- Fuyuki Saito,
- Irina Rogozhina,
- Jane Lund Andersen,
- Moto Kawamata,
- Motohiro Hirabayashi,
- Nathaniel A. Lifton,
- Ola Fredin,
- Jonathan M. Harbor,
- Arjen P. Stroeven,
- Ayako Abe-Ouchi
Affiliations
- Yusuke Suganuma
- National Institute of Polar Research
- Heitaro Kaneda
- Department of Civil and Environmental Engineering, Chuo University
- Martim Mas e Braga
- Geomorphology and Glaciology, Department of Physical Geography, Stockholm University
- Takeshige Ishiwa
- National Institute of Polar Research
- Takushi Koyama
- Department of Geography, Oita University
- Jennifer C. Newall
- Geomorphology and Glaciology, Department of Physical Geography, Stockholm University
- Jun’ichi Okuno
- National Institute of Polar Research
- Takashi Obase
- Atmosphere Ocean Research Institute, University of Tokyo
- Fuyuki Saito
- Japan Agency for Marine-Earth Science and Technology
- Irina Rogozhina
- Department of Geography, Norwegian University of Science and Technology
- Jane Lund Andersen
- Geomorphology and Glaciology, Department of Physical Geography, Stockholm University
- Moto Kawamata
- National Institute of Polar Research
- Motohiro Hirabayashi
- National Institute of Polar Research
- Nathaniel A. Lifton
- Department of Earth, Atmospheric, and Planetary Sciences, Purdue University
- Ola Fredin
- Department of Geoscience and Petroleum, Norwegian University of Science and Technology
- Jonathan M. Harbor
- Geomorphology and Glaciology, Department of Physical Geography, Stockholm University
- Arjen P. Stroeven
- Geomorphology and Glaciology, Department of Physical Geography, Stockholm University
- Ayako Abe-Ouchi
- National Institute of Polar Research
- DOI
- https://doi.org/10.1038/s43247-022-00599-z
- Journal volume & issue
-
Vol. 3,
no. 1
pp. 1 – 11
Abstract
Regional sea-level highstand triggered rapid Holocene upstream thinning of the East Antarctic Ice Sheet in Dronning Maud Land, suggest ice sheet and crustal rebound model simulations constrained by cosmogenic nuclide chronometry.
