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

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Mineral Dust Variability in Antarctic Ice for Different Climate Conditions,rn Hemisphere dust emission, but changes in atmospheric transport are also relevant. The maximum dust deposition in Antarctica is simulated for the LGM, showing a 10-fold increase compared to preindustrial conditions.

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,Vegetation, Climate, Man—Holocene Variability in Monsoonal Central Asia,tantial vegetation changes are confined to the fringe zone of the Asian monsoon area and to the Tibetan Plateau, where simulated forest fraction has decreased by approx. 15 % and 30 % since mid-Holocene, respectively.

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Holocene Climate Dynamics, Biogeochemical Cycles and Ecosystem Variability in the Eastern Mediterrasoxic to anoxic conditions with onset of S1 deposition. The recovery of benthic ecosystems during the terminal S1 phase was controlled by increasingly deeper convection and re-ventilation over a period of approximately 1,500 years.

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证实

Climate Sensitivity During and Between Interglacials,e climate optimum”. IG sensitivities are found to be comparable to estimates for the instrumental period; warming or cooling phases during Marine Isotope Stage (MIS) 5 or 11 do not show significant differences in climate sensitivity.

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