Late Glacial to Holocene dune development at southern Krakower See
Sebastian Lorenz
CORRESPONDING AUTHOR
Universität Greifswald, Institut für Geographie and Geologie, Friedrich-Ludwig-Jahn-Straße 16–17, 17487 Greifswald, Germany
Henrik Rother
Landesamt für Geologie und Bergwesen Sachsen-Anhalt, Köthener Straße 38, 06118 Halle, Germany
Michael Kenzler
Universität Greifswald, Institut für Geographie and Geologie, Friedrich-Ludwig-Jahn-Straße 16–17, 17487 Greifswald, Germany
Sara Kaphengst
Universität Greifswald, Institut für Geographie and Geologie, Friedrich-Ludwig-Jahn-Straße 16–17, 17487 Greifswald, Germany
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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.
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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.
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Geological glacial features such as moraines can be used to construct the environment of former times. While sands may indicate colder phases, soils and peat preserved witness warm phases. Using various dating techniques, the ages of such features can be obtained. This is important in order to get an understanding of the climate of the past, in this study on the extent of the ice marginal position in Schleswig-Holstein.
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