Deglacial ice sheet meltdown: orbital pacemaking and CO<sub>2</sub> effects

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 &sim;25–10 thousand years before present (ka BP), when ice sheets receded quickly and multi-proxy reconstructed global mean surface temperatures rose by &sim;3–5 °C. It still remains unresolved whether insolation changes due...

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Bibliographic Details
Main Authors:	M. Heinemann, A. Timmermann, O. Elison Timm, F. Saito, A. Abe-Ouchi
Format:	Article
Language:	English
Published:	Copernicus Publications 2014-08-01
Series:	Climate of the Past
Online Access:	http://www.clim-past.net/10/1567/2014/cp-10-1567-2014.pdf

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