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

征兵

Holocene Environmental Variability in the Arctic Gateway,ow a consistently high freshwater input to the Arctic Ocean during the last 7 ka. The signal is robust against the Holocene cooling trend, however sensitive towards the warming trend of the last century. These results may play a role in the observed Arctic changes.

细查

Detecting Holocene Changes in the Atlantic Meridional Overturning Circulation: Integration of Proxyof central water circulation in communicating regional climate signatures of various forcings (freshwater flux, solar variability, orbital parameters) onto a hemispheric or global scale via cross-gyre meridional heat transfer from high to low latitudes.

braggadocio

Hydroclimatic Variability in the Panama Bight Region During Termination 1 and the Holocene,ns during H1, capture this precipitation dipole, while showing no change in the Atlantic-to-Pacific water vapor flux in response to a slowdown of the Atlantic meridional overturning circulation (AMOC). We conclude that the cross-isthmus vapor flux feedback on AMOC variations is negligible.

Jubilation

The Southern Westerlies During the Holocene: Paleoenvironmental Reconstructions from Chilean Lake, om the mid- to late Holocene are not yet consistent with these proxy results. However, a good data-model agreement exists when investigating the potential impact of solar variability on the SWW at centennial time-scales during the latest Holocene with periods of lower (higher) solar activity causing equatorward (southward) shifts of the SWW.

极端的正确性

悲观

North-West African Hydrologic Changes in the Holocene: A Combined Isotopic Data and Model Approach,imentary plant waxes show no abrupt change at the end of the AHP suggesting a gradual precipitation decline. These results are supported by Holocene climate simulations using a coupled atmosphere-land surface model, which includes an explicit modeling of isotopic fractionation within the hydrological cycle.

Abnormal

Comparison of Climate and Carbon Cycle Dynamics During Late Quaternary Interglacials,ement. The carbon cycle dynamics during MIS 11.3 can generally be explained by the same forcing mechanisms as for the Holocene, while model and data disagree during MIS 5.5, showing an increasing CO. trend in the model though reconstructions are constant.

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,DFG Priority Research Program “Integrated Analysis of Interglacial Climate Dynamics” (INTERDYNAMIC)e reliable scenarios for future climate change. Between 2006 and 2013 a total of 22 projects were funded by the . (DFG) in this framework. The purpose of this book is to provide an overview of the key findings and a guide to the publications that resulted from each project.

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