A model-tested North Atlantic Oscillation reconstruction for the past millennium

Pablo Ortega (), Flavio Lehner, Didier Swingedouw, Valerie Masson-Delmotte, Christoph C. Raible, Mathieu Casado and Pascal Yiou
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Pablo Ortega: LSCE/IPSL, UMR 8212 (CEA-CNRS-UVSQ)
Flavio Lehner: Climate and Environmental Physics, Physics Institute, University of Bern
Didier Swingedouw: EPOC, Université Bordeaux 1
Valerie Masson-Delmotte: LSCE/IPSL, UMR 8212 (CEA-CNRS-UVSQ)
Christoph C. Raible: Climate and Environmental Physics, Physics Institute, University of Bern
Mathieu Casado: LSCE/IPSL, UMR 8212 (CEA-CNRS-UVSQ)
Pascal Yiou: LSCE/IPSL, UMR 8212 (CEA-CNRS-UVSQ)

Nature, 2015, vol. 523, issue 7558, 71-74

Abstract: The North Atlantic Oscillation (NAO) is an important source of climate variability in the Northern Hemisphere; here, a model-tested reconstruction of the NAO for the past millennium reveals that positive NAO phases were predominant during the thirteenth and fourteenth centuries, but not during the whole medieval period.

Date: 2015
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DOI: 10.1038/nature14518

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