Research article 09 Oct 2015
Research article | 09 Oct 2015
Obliquity forcing of low-latitude climate
J. H. C. Bosmans et al.
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Cited
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39 citations as recorded by crossref.
- Astronomical calibration and global correlation of the Santonian (Cretaceous) based on the marine carbon isotope record N. Thibault et al. 10.1002/2016PA002941
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- Bispectra of climate cycles show how ice ages are fuelled D. Liebrand & A. de Bakker 10.5194/cp-15-1959-2019
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- Heterodynes dominate precipitation isotopes in the East Asian monsoon region, reflecting interaction of multiple climate factors E. Thomas et al. 10.1016/j.epsl.2016.09.044
- Responses of global monsoon and seasonal cycle of precipitation to precession and obliquity forcing Z. Ding et al. 10.1007/s00382-021-05663-6
- Self-sustained oscillations and global climate changes L. Arnaut & S. Ibáñez 10.1038/s41598-020-68052-9
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Latest update: 26 Feb 2021
Short summary
Our study shows that the influence of obliquity (the tilt of Earth's rotational axis) can be explained through changes in the insolation gradient across the tropics. This explanation is fundamentally different from high-latitude mechanisms that were previously often inferred to explain obliquity signals in low-latitude paleoclimate records, for instance glacial fluctuations. Our study is based on state-of-the-art climate model experiments.
Our study shows that the influence of obliquity (the tilt of Earth's rotational axis) can be...