Carbon dioxide levels are linked to Milankovitch cycles in ice core data
Ice core data and paleoclimate modeling demonstrate that atmospheric carbon dioxide levels are closely coupled with glacial cycles paced by Milankovitch orbital forcing.
The retrieved scientific literature consistently supports the link between carbon dioxide levels and Milankovitch orbital cycles as observed in ice core and paleoclimate proxy data. Multiple papers examine how orbital forcing drives glacial cycles and how carbon dioxide acts as a key feedback or amplification mechanism within these cycles.
N. Keyes, L. T. Giorgini, J. Wettlaufer. Stochastic paleoclimatology: Modeling the EPICA ice core climate records.. 2022. https://doi.org/10.1063/5.0128814
Analyzes 800 kiloyears of EPICA ice core data to examine the coupling of carbon dioxide and temperature during Pleistocene glacial cycles.
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C. Xiao, Z. Du, M. Handley, P. Mayewski, Junji Cao, S. Schüpbach, Tong Zhang, J. Petit, Chuanjin Li, Yeongcheol Han, Yuefang Li, Jiawen Ren. Iron in the NEEM ice core relative to Asian loess records over the last glacial–interglacial cycle. 2020. https://doi.org/10.1093/nsr/nwaa144
Indicates that variations in mineral dust input and carbon dioxide relationships in the NEEM ice core are driven by solar radiation changes in response to Earth's orbital cycles.
A. Ganopolski, R. Calov. The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles. 2011. https://doi.org/10.5194/cpd-7-2391-2011
Demonstrates that temporal variability in atmospheric carbon dioxide plays an important role in the amplification of 100-kyr glacial cycles synchronized with orbital eccentricity.
Gerald E. Marsh. Interglacials, Milankovitch Cycles, Solar Activity, and Carbon Dioxide. 2014. https://doi.org/10.1155/2014/345482
Notes the established understanding that interglacial periods are initiated by Milankovitch cycles enhanced by rising atmospheric carbon dioxide concentrations.
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