Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica

• Main Authors: Turney, Chris S.M., Fogwill, Christopher J., Golledge, Nicholas R., McKay, Nicholas P., van Sebille, Erik, Jones, Richard T., Etheridge, David, Rubino, Mauro, Thornton, David P., Davies, Siwan M., Ramsey, Christopher Bronk, Thomas, Zoë A., Bird, Michael I., Munksgaard, Niels C., Kohno, Mika, Woodward, John, Winter, Kate, Weyrich, Laura S., Rootes, Camilla M., Millman, Helen, Albert, Paul G., Rivera, Andres, van Ommen, Tas, Curran, Mark, Moy, Andrew, Rahmstorf, Stefan, Kawamura, Kenji, Hillenbrand, Claus-Dieter, Weber, Michael E., Manning, Christina J., Young, Jennifer, Cooper, Alan
• Format: Article in Journal/Newspaper
• Language: English
• Published: Washington, DC : National Acad. of Sciences 2020
• Subjects: Antarctic ice sheets; Marine ice sheet instability (MISI); Paleoclimatology; Polar amplification; Tipping element; 000; 500; Antarctic; Southern Ocean; The Antarctic; Weddell Sea; West Antarctic Ice Sheet; Greenland; Weddell; Misi; Antarc*; Antarctica; Ice Sheet; Methane hydrate; North Atlantic
• Online Access: https://oa.tib.eu/renate/handle/123456789/7732; https://doi.org/10.34657/6779

The future response of the Antarctic ice sheet to rising temperatures remains highly uncertain. A useful period for assessing the sensitivity of Antarctica to warming is the Last Interglacial (LIG) (129 to 116 ky), which experienced warmer polar temperatures and higher global mean sea level (GMSL) (...