Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-2143-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-20-2143-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 Sep 2024
Research article |
| 26 Sep 2024
| 26 Sep 2024
North Atlantic Oscillation polarity during the past 3000 years derived from sediments of a large lowland lake, Schweriner See, in NE Germany
Marie-Luise Adolph
CORRESPONDING AUTHOR
Department of Physical Geography, Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
Sambor Czerwiński
Department of Physical Geography, Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University in Poznań, Poznań, Poland
Department of Geomorphology and Quaternary Geology, University of Gdańsk, Gdańsk, Poland
Mirko Dreßler
Department of Physical Geography, Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
Paul Strobel
Department of Physical Geography, Institute for Geography, Friedrich Schiller University Jena, Jena, Germany
Marcel Bliedtner
Department of Physical Geography, Institute for Geography, Friedrich Schiller University Jena, Jena, Germany
Sebastian Lorenz
Department of Physical Geography, Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
Maxime Debret
UMR 6143 M2C Laboratoire Morphodynamique Continentale et Côtière, Department of Geoscience, Université de Rouen Normandie, Rouen, France
Torsten Haberzettl
Department of Physical Geography, Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
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Short summary
We reconstruct environmental changes derived from sediments of Schweriner See, a large lake in NE Germany, for the past 3000 years. We infer variations in North Atlantic large-scale atmospheric circulation systems, namely the North Atlantic Oscillation (NAO), by combining sedimentological, geochemical, and biological parameters. Our results suggest distinct shifts between positive and negative NAO phases affecting winter temperatures, precipitation, and westerly wind strength at our study site.
We reconstruct environmental changes derived from sediments of Schweriner See, a large lake in...
