Regional imprints of millennial variability during the MIS 3 period around Antarctica

• Published in: Quaternary Science Reviews
• Main Authors: Buiron D., J. Chappellaz, A. Landais, M. Baumgartner, E. Capron, M. Frezzotti, M. Kageyama, B. Lemieux Dudon, V. Masson Delmotte, F. Parrenin, A. Schilt, E. Selmo, M. Severi, D. Swingedouw, R. Udisti, STENNI, BARBARA, BONAZZA, MATTIA
• Other Authors: Buiron, D., Stenni, Barbara, J., Chappellaz, A., Landai, M., Baumgartner, Bonazza, Mattia, E., Capron, M., Frezzotti, M., Kageyama, B., Lemieux Dudon, V., Masson Delmotte, F., Parrenin, A., Schilt, E., Selmo, M., Severi, D., Swingedouw, R., Udisti
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2012
• Subjects: Paleoclimate; millennial-scale variability; glacial period; ice core; Talos Dome; global coupled model simulations; Antarctic; Southern Ocean; Greenland; Pacific; Indian; Antarc*; Antarctica; Greenland ice cores; North Atlantic
• Online Access: http://hdl.handle.net/11368/2626920; https://doi.org/10.1016/j.quascirev.2012.05.023

The climate of the last glacial Marine Isotopic Stage 3 (MIS3) period is characterized by strong millennialscale variability with a succession of DansgaardeOeschger events first identified in Greenland ice cores and associated with variations of the Atlantic Meridional Overturning Circulation (AMOC)...