Effect of the Ordovician paleogeography on the (in)stability of the climate
The Ordovician Period (485–443 Ma) is characterized by abundant evidence for continental-sized ice sheets. Modeling studies published so far require a sharp CO<sub>2</sub> drawdown to initiate this glaciation. They mostly used non-dynamic slab mixed-layer ocean models. Here, we us...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-11-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/10/2053/2014/cp-10-2053-2014.pdf |