Deglacial ice sheet meltdown: orbital pacemaking and CO<sub>2</sub> effects
One hundred thousand years of ice sheet buildup came to a rapid end ∼25–10 thousand years before present (ka BP), when ice sheets receded quickly and multi-proxy reconstructed global mean surface temperatures rose by ∼3–5 °C. It still remains unresolved whether insolation changes due...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-08-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/10/1567/2014/cp-10-1567-2014.pdf |