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

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) (...

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Veröffentlicht in:	Proceedings of the National Academy of Sciences - PNAS 2020-02, Vol.117 (8), p.3996-4006
Hauptverfasser:	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, Zoe 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:	Artikel
Sprache:	eng
Schlagworte:	Deoxyribonucleic acid Destabilization DNA Environmental changes Glaciers Hydrates Ice Ice sheets Methane hydrates Microorganisms Mountains Ocean models Ocean temperature Ocean warming Physical Sciences PNAS Plus Polar environments Sea level Sea level changes Sheet modelling Thermal expansion Water circulation
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