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Multiple sources of atmospheric CO2 activated by AMOC recovery at the onset of interglacial MIS 9 Proceedings of the National Academy of Sciences of the United States of America, 2025
(Ref: 17321)
Authors:
Category 1: Peer-reviewed literature
Using high-precision ice core measurements of CO2, ?13C-CO2, CH4, and N2O, this study provides carbon isotope constraints on a sizeable, centennial-scale CO2 jump at the onset of Marine Isotope Stage 9 (MIS 9). The very end of the Heinrich stadial (HS) characterizing Termination IV (T-IV, ca.
The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature Geophysical Research Letters, 2023
(Ref: 16752)
Category 1: Peer-reviewed literature
Technical Summary Climate Change 2007: The Physical Science Basis. Contribution of Working Group 1 to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, 2007
(Ref: 13241)
Authors:
Solomon S.Qin D.Manning M.Alley R.B.Berntsen T.Bindoff N.L.Chen Z.Chidthaisong A.Gregory J.M.Hegerl G.C.Heimann M.Hewitson B.Hoskins B.J.Joos F.Jouzel J.Kattsov V.Lohmann U.Matsuno T.Molina M.Nicholls N.Overpeck J.Raga G.Ramaswamy V.Ren J.Rusticucci M.Somerville R.Stocker T.F.Whetton P.Wood R.A.Wratt D.
Category 1: Peer-reviewed literature
The 8200 B.P. climate event in the Southern Hemisphere Geophysical Research Abstracts, 2007
(Ref: 12863)
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Category 3: Abstract
The 8200 B.P. climate event in the Southern Hemisphere Antarctic Climate and Ecosystems CRC Symposium, Hobart, 2007, 2007
(Ref: 13162)
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Category 3: Conference paper
The event that occurred approximately 8200 years ago is the largest excursion in climate since the beginning of the Holocene. In this event we observe the climatic response to a perturbation which provides a probe with which to investigate the stability of interglacial climate.