Antarctic Ice Sheet re-advance during the Antarctic Cold Reversal identified in the Western Ross Sea

• Main Authors: Baroni C., Tenti M., Bart P. J., Salvatore M. C., Gasperini L., Busetti M., Sauli C., Stucchi E. M., Tognarelli A.
• Other Authors: Baroni, C., Tenti, M., Bart, P. J., Salvatore, M. C., Gasperini, L., Busetti, M., Sauli, C., Stucchi, E. M., Tognarelli, A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2022
• Subjects: Drygalski Basin; Seafloor geomorphology; Geophysical data; Deglaciation; Antarctic Cold Reversal; AIS Re-advance; Antarctica; Antarctic; Coulman Island; Drygalski; Ross Sea; The Antarctic; Antarc*; Ice Sheet
• Online Access: https://hdl.handle.net/11568/1184450; https://doi.org/10.4461/GFDQ.2022.45.1; http://gfdq.glaciologia.it/045_1_01_2022/

Marine geophysical data collected from the Ross Sea continental shelf during several oceanographic expeditions enabled evaluation of the Last Glacial Maximum (LGM) extent of the Antarctic Ice Sheet (AIS) through the presence of large Grounding Zone Wedges (GZWs), particularly evident in the outer re...