Project Details
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Quantification of Past Ocean Dynamics.

Applicant Dr. Jörg Lippold
Subject Area Palaeontology
Mineralogy, Petrology and Geochemistry
Oceanography
Term from 2016 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 277128673
 
Final Report Year 2023

Final Report Abstract

The Atlantic meridional overturning circulation (AMOC) represents a potentially vulnerable component of the climate system. A forthcoming collapse of the AMOC under anthropogenic greenhouse forcing is thus a major concern. In order to enhance our understanding of the AMOC behaviour, the main goal of the project was to reconstruct past ocean dynamics by providing quantitative estimates from both proxy observations and model attempts. Here, the temporal focus of the investigations was set on the last glacial, the deglacial period, and the Holocene. In a first step, improvements of the proxy methodologies were implemented followed by intensive acquisition of observational proxy data with focus on the kinematic 231Pa/230Th circulation proxy and the εNd water mass tag. This new database served as the starting point for better understanding of AMOC-related and AMOC-unrelated processes influencing the proxies. As a main objective, this new database allowed for identifying the most likely AMOC scenarios for the variable climate conditions of the past by applying the Bern3D climate model. We found a shallow and weak Atlantic overturning circulation during the Last Glacial Maximum reconciling former and apparently conflicting proxy evidence. Model–data comparison of the last deglaciation indicates a highly variable AMOC, strongly dependent on the climatic and oceanic background state. In contrast, no significant variations were observed for the whole Holocene and yet during distinct climatic events within the last ~10,000 years, despite extraordinary high temporal observational sample resolution.

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