Spectrum of 100-kyr glacial cycle: Orbital inclination, not eccentricity
Spectral analysis of climate data shows a strong narrow peak with period ≈100 kyr, attributed by the Milankovitch theory to changes in the eccentricity of the earth’s orbit. The narrowness of the peak does suggest an astronomical origin; however the shape of the peak is incompatible with both linear...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
1997
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC33747/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607741/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.94.16.8329 |
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