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A long-term numerical solution for the insolation quantities of the Earth
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“This external or exogenic forcing is known as the orbital pacing of the climate system, and it regulates the amount of incoming solar radiation on the planet’s surface as well as its distribution across latitude, affecting the length and intensity of the seasons.”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [1]
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“Subtle, quasiperiodic changes in Earth’s orbit around the sun are caused by gravitational interactions of larger celestial bodies in the solar system (1).”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [1]
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“For avoiding circular reasoning and allowing to extract characteristic patterns of eccentricity embedded in the records, it was suggested to use a simple cosine function for intervals older than 60 Ma (1, 72).”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [1]
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“However, to establish an astrochronology, the stable long eccentricity cycle with a period of ~405 kyr can be used (1, 72).”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [1]
In the citing paper
“Late Maastrichtian records from around the world are well-known to be dominated by this orbital cycle (22–24), which, at about 67 Ma, had an average periodicity of ~20.4 kyr (1).”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [1]
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Long term evolution and chaotic diffusion of the insolation quantities of Mars
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Cited by
Long term evolution and chaotic diffusion of the insolation quantities of Mars
Laskar, J., Correia, A. C. M., Gastineau, M., Joutel, F., Levrard, B., & Robutel, P. (2004) · Icarus · doi:10.1016/j.icarus.2004.04.005 · Cited by 992
Self-citationInterglacials of the last 800,000 years
Past Interglacials Working Group of PAGES (2016) · Reviews of Geophysics · doi:10.1002/2015rg000482 · Cited by 606
Climate forcing reconstructions for use in PMIP simulations of the last millennium (v1.0)
Schmidt, G. A., Jungclaus, J. H., Ammann, C. M., Bard, E., Braconnot, P., Crowley, T. J., Delaygue, G., Joos, F., Krivova, N. A., Muscheler, R., et al. (2011) · Geoscientific Model Development · doi:10.5194/gmd-4-33-2011 · Cited by 499
Fletcher, W. J., & Sánchez Goñi, M. F. (2008) · Quaternary Research · doi:10.1016/j.yqres.2008.07.002 · Cited by 399
Dynamics of Green Sahara Periods and Their Role in Hominin Evolution
Larrasoaña, J. C., Roberts, A. P., & Rohling, E. J. (2013) · PLoS ONE · doi:10.1371/journal.pone.0076514 · Cited by 334
Metadata
- Authors
- Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., & Levrard, B.
- Venue
- Astronomy & Astrophysics
- Publisher
- EDP Sciences
- Published
- 2004-11-23
- Volume
- 428
- Issue
- 1
- Pages
- 261-285
- ISSN
- 0004-6361
- 1432-0746
- Cited by
- 3,837
- References
- 1
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- Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., & Levrard, B. (2004). A long-term numerical solution for the insolation quantities of the Earth. Astronomy & Astrophysics. https://doi.org/10.1051/0004-6361%3A20041335
