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...

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Bibliographic Details
Main Authors: Y. Milker, R. Rachmayani, M. F. G. Weinkauf, M. Prange, M. Raitzsch, M. Schulz, M. Kučera
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/9/2231/2013/cp-9-2231-2013.pdf

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