Atmospheric circulation over Europe during the Younger Dryas

Author:

Rea Brice R.1ORCID,Pellitero Ramón2ORCID,Spagnolo Matteo1ORCID,Hughes Philip3ORCID,Ivy-Ochs Susan4,Renssen Hans5ORCID,Ribolini Adriano6ORCID,Bakke Jostein7,Lukas Sven8ORCID,Braithwaite Roger J.3

Affiliation:

1. School of Geosciences University of Aberdeen, Aberdeen, UK.

2. Departamento de Geografía, Universidad Nacional de Educación a Distancia (UNED), Madrid, Spain.

3. Department of Geography, University of Manchester, Manchester, UK.

4. Laboratory of Ion Beam Physics, ETH Zürich, 8093 Zürich, Switzerland.

5. Department of Natural Sciences and Environmental Health, University of South-Eastern Norway, Bø, Norway.

6. Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 53, 56126, Pisa, Italy.

7. Department of Earth Science, University of Bergen, P.O. Box 7800 5020 Bergen, Norway.

8. Department of Geology, Lund University, Sölvegatan 12, Lund, Sweden.

Abstract

Reconstructed palaeoprecipitation reveals a persistent SCAND-like circulation and southerly storm track during the Younger Dryas.

Funder

Leverhulme Trust

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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