The precession of Earth's apses significantly affects long-term climate patterns
The precession of Earth's apses (as part of orbital forcing/Milankovitch cycles) significantly impacts long-term climate patterns, glaciation, and paleoclimate records.
The retrieved papers provide robust paleoclimatic and theoretical support establishing that orbital forcing parameters, including Earth's precession, heavily influence long-term climate cycles, regional precipitation, and glacial terminations.
Xiaojuan Liu, David S. Battisti. The Influence of Orbital Forcing of Tropical Insolation on the Climate and Isotopic Composition of Precipitation in South America. 2015. https://doi.org/10.1175/jcli-d-14-00639.1
Demonstrates how orbital forcing, which includes precession, significantly changes regional climate patterns and precipitation by altering insolation.
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A. Ganopolski. Toward generalized Milankovitch theory (GMT). 2024. https://doi.org/10.5194/cp-20-151-2024
Discusses the extended Milankovitch theory, confirming that orbital parameters including precession heavily dictate Quaternary glacial-interglacial cycles.
Yuyin Li, He Huang, Yuan Gao, Yongqiang Cao, Hu Cheng, Chenlu Hei, Shuang Liang. The ∼170 kyr astronomical cycle in the Early Permian Lucaogou Formation of the Junggar Basin. 2024. https://doi.org/10.3389/feart.2024.1272857
Identifies precession cycles within geological formations, linking them to periodic paleoclimate and carbon cycle modifications.
F. Marra. Cumulated insolation: a simple explanation of Milankovitch's forcing on climate changes. 2013. https://doi.org/10.5194/cpd-9-5553-2013
Explains how Milankovitch's orbital forcing parameters drive significant historical climate changes and glacial terminations.
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