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Proceedings of the National Academy of Sciences of the United States of America|June 2, 2025
Multiple sources of atmospheric CO2 activated by AMOC recovery at the onset of interglacial MIS 9Florian Krauss, Daniel Baggenstos, Jochen Schmitt, et al.Nature|December 16, 2014
Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciationAdrian Schilt, Edward J Brook, Thomas K Bauska, et al.Scientific Reports|January 6, 2025
Rapid climate action is needed: comparing heat vs. COVID-19-related mortalityFulden Batibeniz, Sonia I Seneviratne, Srinidhi Jha, et al.Proceedings of the National Academy of Sciences of the United States of America|June 24, 2020
Extreme climate after massive eruption of Alaska's Okmok volcano in 43 BCE and effects on the late Roman Republic and Ptolemaic KingdomJoseph R McConnell, Michael Sigl, Gill Plunkett, et al.Proceedings of the National Academy of Sciences of the United States of America|May 13, 2024
Southern Ocean drives multidecadal atmospheric CO2 rise during Heinrich StadialsKathleen A Wendt, Christoph Nehrbass-Ahles, Kyle Niezgoda, et al.Nature|January 29, 2025
The Ronne Ice Shelf survived the last interglacialEric W Wolff, Robert Mulvaney, Mackenzie M Grieman, et al.Nature|November 18, 2024
Geological Net Zero and the need for disaggregated accounting for carbon sinksMyles R Allen, David J Frame, Pierre Friedlingstein, et al.Nature|June 11, 2004
Eight glacial cycles from an Antarctic ice coreLaurent Augustin, Carlo Barbante, Piers R F Barnes, et al.Pageof 4