Global and regional sea surface temperature trends during Marine Isotope Stage 11
The Marine Isotope Stage (MIS) 11 (424–374 ka) was characterized by a protracted deglaciation and an unusually long climatic optimum. It remains unclear to what degree the climate development during this interglacial reflects the unusually weak orbital forcing or greenhouse gas trends. Previously, a...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-10-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/9/2231/2013/cp-9-2231-2013.pdf |