Articles | Volume 9, issue 3
https://doi.org/10.5194/tc-9-881-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-881-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Simulating the Antarctic ice sheet in the late-Pliocene warm period: PLISMIP-ANT, an ice-sheet model intercomparison project
B. de Boer
CORRESPONDING AUTHOR
Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, the Netherlands
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Utrecht, the Netherlands
A. M. Dolan
School of Earth and Environment, University of Leeds, Leeds, UK
J. Bernales
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Freie Universitaet Berlin, Berlin, Germany
E. Gasson
Climate System Research Center, University of Massachusetts Amherst, Amherst, Massachusetts, USA
H. Goelzer
Earth System Sciences & Departement Geografie, Vrije Universiteit Brussel, Brussels, Belgium
N. R. Golledge
Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
GNS Science, Avalon, 5011 Lower Hutt, New Zealand
J. Sutter
Alfred Wegener Institute, Bremerhaven, Germany
P. Huybrechts
Earth System Sciences & Departement Geografie, Vrije Universiteit Brussel, Brussels, Belgium
G. Lohmann
Alfred Wegener Institute, Bremerhaven, Germany
I. Rogozhina
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
A. Abe-Ouchi
Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, 277-8568, Japan
Department of Integrated Climate Change Projection Research, JAMSTEC, Yokohama, Japan
R. S. W. van de Wal
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Utrecht, the Netherlands
Viewed
Total article views: 7,270 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 05 Nov 2014)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 4,165 | 2,828 | 277 | 7,270 | 696 | 286 | 345 |
- HTML: 4,165
- PDF: 2,828
- XML: 277
- Total: 7,270
- Supplement: 696
- BibTeX: 286
- EndNote: 345
Total article views: 6,088 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 May 2015)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 3,476 | 2,363 | 249 | 6,088 | 407 | 262 | 324 |
- HTML: 3,476
- PDF: 2,363
- XML: 249
- Total: 6,088
- Supplement: 407
- BibTeX: 262
- EndNote: 324
Total article views: 1,182 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 05 Nov 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 689 | 465 | 28 | 1,182 | 24 | 21 |
- HTML: 689
- PDF: 465
- XML: 28
- Total: 1,182
- BibTeX: 24
- EndNote: 21
Latest update: 27 Nov 2025
Short summary
We present results from simulations of the Antarctic ice sheet by means of an intercomparison project with six ice-sheet models. Our results demonstrate the difficulty of all models used here to simulate a significant retreat or re-advance of the East Antarctic ice grounding line. Improved grounding-line physics could be essential for a correct representation of the migration of the grounding line of the Antarctic ice sheet during the Pliocene.
We present results from simulations of the Antarctic ice sheet by means of an intercomparison...