Dynamic behaviour of the East Antarctic ice sheet during Pliocene warmth

By C. Cook, T. Flierdt, T. Williams, S. Hemming, M. Iwai, M. Kobayashi, F. Jiménez-Espejo, C. Escutia, J. Gonzàlez, B. Khim and 32 more. 2013

292 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/35d243b9f7ecff71bbafc53e0aecbf4f7c7f7316

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Robert M. DeConto
2. Stefan Rahmstorf
3. M. Raymo
4. G. Milne
5. P. Whitehouse
6. David D. Pollard

In Ecology

1. Robert M. DeConto
2. Stefan Rahmstorf
3. David D. Pollard

Citations in the corpus

• Contribution of Antarctica to past and future sea-level rise (2016, unknown): “Surface meltwater may lead to the ultimate demise of the major buttressing ice shelves (Supplementary Videos 8 and 9) and extensive grounding-line retreat, but it is the long thermal memory of the ocean that will inhibit the recovery of marine-based ice for thousands of years after greenhouse gas…”
• Sea-level rise due to polar ice-sheet mass loss during past warm periods (2015, background): “Studies of ice-rafted debris (IRD) suggest that portions of the East Antarctic Ice Sheet (EAIS) experienced retreat during parts of the early to middle Pliocene (20), apparently paced by precessional (23-ky) cycles (21).”