Workshop report
| 
25 Feb 2022
Workshop report |
| 25 Feb 2022
| 25 Feb 2022
Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
Molly O. Patterson
CORRESPONDING AUTHOR
Department of Geological Sciences and Environmental Studies, Binghamton University, Binghamton, NY, USA
Richard H. Levy
GNS Science, Lower Hutt, New Zealand
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Denise K. Kulhanek
Department of Geological Sciences and Environmental Studies, Binghamton University, Binghamton, NY, USA
Institute of Geosciences, Christian-Albrecht University of Kiel, Kiel, Germany
Tina van de Flierdt
Department of Earth Science and Engineering, Imperial College London, London, UK
Huw Horgan
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Gavin B. Dunbar
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Timothy R. Naish
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Jeanine Ash
Department of Earth, Environmental and Planetary Sciences, Rice
University, Houston, TX, USA
Alex Pyne
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Darcy Mandeno
Antarctic Research Centre, Victoria University of Wellington,
Wellington, New Zealand
Paul Winberry
Department of Geological Sciences, Central Washington University,
Ellensburg, WA, USA
David M. Harwood
Department of Earth & Atmospheric Sciences, University of
Nebraska-Lincoln, Lincoln, NE, USA
Fabio Florindo
Instituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
Francisco J. Jimenez-Espejo
Instituto Andaluz de Ciencias de la Tierra, Spanish Research Council (CSIC), Armilla, Spain
Andreas Läufer
Federal Institute for Geosciences and Natural Resources (BGR),
Hannover, Germany
Kyu-Cheul Yoo
Division of Glacial Environment Research, Korea Polar Research
Institute, Incheon, Republic of Korea
Osamu Seki
National Institute of Polar Research, 10-3 Midori-cho, Tachikawa,
Tokyo, Japan
Institute of Low Temperature Science, Hokkaidō University,
Sapporo, Japan
Paolo Stocchi
Department of Coastal Systems, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, the Netherlands
Johann P. Klages
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
Jae Il Lee
Division of Glacial Environment Research, Korea Polar Research
Institute, Incheon, Republic of Korea
Florence Colleoni
Istituto Nazionale di Oceanografia e Geofisica Sperimentale, Trieste, Italy
Yusuke Suganuma
National Institute of Polar Research, 10-3 Midori-cho, Tachikawa,
Tokyo, Japan
Edward Gasson
School of Geographical Sciences, University of Bristol, Bristol, UK
Christian Ohneiser
Department of Geology, University of Otago, Dunedin, New Zealand
José-Abel Flores
Department of Geology, University of Salamanca, Salamanca, Spain
David Try
GNS Science, Lower Hutt, New Zealand
Rachel Kirkman
GNS Science, Lower Hutt, New Zealand
Daleen Koch
GNS Science, Lower Hutt, New Zealand
A full list of authors appears at the end of the paper.
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Cited
4 citations as recorded by crossref.
- Return to the Ross Ice Shelf Project (RISP), Site J-9 (1977–1979): perspectives of West Antarctic Ice Sheet history from Miocene and Holocene benthic foraminifera S. Dameron et al. 10.5194/jm-43-187-2024
- Geomorphology and shallow sub-sea-floor structures underneath the Ekström Ice Shelf, Antarctica A. Oetting et al. 10.5194/tc-16-2051-2022
- Population morphometrics of the Southern Ocean diatom Fragilariopsis kerguelensis related to sea surface temperature J. Ruggiero et al. 10.5194/jm-43-323-2024
- Evaluating and locating a suitable bedrock drilling site near zhongshan station with airborne and ground-based observations Y. Li et al. 10.1016/j.polar.2024.101076
Latest update: 12 Nov 2024
Short summary
How much of the West Antarctic Ice Sheet will melt and how quickly it will happen when average global temperatures exceed 2 °C is currently unknown. Given the far-reaching and international consequences of Antarctica’s future contribution to global sea level rise, the SWAIS 2C Project was developed in order to better forecast the size and timing of future changes.
How much of the West Antarctic Ice Sheet will melt and how quickly it will happen when average...
