Pleistocene glacial variability as a chaotic response to obliquity forcing
The mid-Pleistocene Transition from 40 ky to ~100 ky glacial cycles is generally characterized as a singular transition attributable to scouring of continental regolith or a long-term decrease in atmospheric CO<sub>2</sub> concentrations. Here an alternative hypothesis is...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2009-09-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/5/481/2009/cp-5-481-2009.pdf |