Titlebook: Integrated Analysis of Interglacial Climate Dynamics (INTERDYNAMIC); Michael Schulz,Andre Paul Book 2015 The Author(s) 2015 Climate Modeli

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Global Synthesis of Sea-Surface Temperature Trends During Marine Isotope Stage 11,m 57 sites. We aligned these records by oxygen-isotope stratigraphy and subjected them to an Empirical Orthogonal Function (EOF) analysis. The principal SST trend (EOF1) reflects a rapid deglacial warming of the surface ocean in pace with carbon dioxide rise during Termination V, followed by a broad

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Evaluation of Eemian and Holocene Climate Trends: Combining Marine Archives with Climate Modelling,he data reveal contrasting SST trends, depending upon the proxy used to derive Holocene SST history. To reconcile these mismatches between proxies in the estimated Holocene SST trends, it has been proposed that the Holocene evolution of orbitally-driven seasonality of the incoming radiation is the f

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Holocene Environmental Variability in the Arctic Gateway,ination of proxy-based paleoceanographic reconstructions as well as transient and time-slice simulations with climate models. Today, the area is perennially ice-covered in the west and ice-free in the east. Results show that sea-ice conditions were highly variable on short timescales in the last 9 k

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Phase-Shift Between Surface Ocean Warming, Evaporation and Changes of Continental Ice Volume Duringg of the northern continental ice masses is lacking behind challenges the Milankovitch theory of climate change and emphasizes the role of the tropics for global climate change. Although the simultaneous multi-proxy approach of planktonic foraminiferal Mg/Ca, δ.O and δ.Ca from tropical sediment core

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Control of Seasonality and Interannual to Centennial Climate Variability in the Caribbean During th Holocene, by using marine (shallow-water corals) and terrestrial (speleothems) climate archives, and climate model simulations (COSMOS). Sea-surface temperature (SST) variability on interdecadal to multidecadal timescales was more pronounced during the mid-Holocene compared to the late Holocene. Th