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

• Published in: Quaternary Science Reviews
• Main Authors: Buiron D., Stenni B., Chappellaz J., Landais A., Baumgartner M., Bonazza M., Capron E., Frezzotti M., Kageyama M., Lemieux-Dudon B., Masson-Delmotte V., Parrenin F., Schilt A., Selmo E., Severi M., Swingedouw D., Udisti R.
• Other Authors: Buiron, D., Stenni, B., Chappellaz, J., Landais, A., Baumgartner, M., Bonazza, M., Capron, E., Frezzotti, M., Kageyama, M., Lemieux-Dudon, B., Masson-Delmotte, V., Parrenin, F., Schilt, A., Selmo, E., Severi, M., Swingedouw, D., Udisti, R.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2012
• Subjects: Glacial period; Global coupled model simulation; Ice core; Millennial-scale variability; Paleoclimate; Talos Dome; Antarctic; Southern Ocean; Greenland; Pacific; Indian; Antarc*; Antarctica; Dansgaard-Oeschger events; Greenland ice cores; ice core; North Atlantic
• Online Access: http://hdl.handle.net/11590/353575; 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 millennial-scale variability with a succession of Dansgaard-Oeschger events first identified in Greenland ice cores and associated with variations of the Atlantic Meridional Overturning Circulation (AMOC...