El Niño modulations over the past seven centuries

Jinbao Li (), Shang-Ping Xie, Edward R. Cook, Mariano S. Morales, Duncan A. Christie, Nathaniel C. Johnson, Fahu Chen, Rosanne D’Arrigo, Anthony M. Fowler, Xiaohua Gou and Keyan Fang
Additional contact information
Jinbao Li: University of Hong Kong
Shang-Ping Xie: International Pacific Research Center, University of Hawaii at Manoa
Edward R. Cook: Lamont-Doherty Earth Observatory, Columbia University, Palisades
Mariano S. Morales: Instituto Argentino de Nivologı´a, Glaciologı´a y Ciencias Ambientales (IANIGLA), CCT-CONICET
Duncan A. Christie: Laboratorio de Dendrocronologı´a y Cambio Global, Instituto de Conservación Biodiversidad y Territorio, Facultad de Ciencias Forestales y Recursos Naturales, Universidad Austral de Chile
Nathaniel C. Johnson: International Pacific Research Center, University of Hawaii at Manoa
Fahu Chen: MOE Key Laboratory of Western China’s Environmental System, Lanzhou University
Rosanne D’Arrigo: Lamont-Doherty Earth Observatory, Columbia University, Palisades
Anthony M. Fowler: School of Environment, The University of Auckland
Xiaohua Gou: MOE Key Laboratory of Western China’s Environmental System, Lanzhou University
Keyan Fang: MOE Key Laboratory of Western China’s Environmental System, Lanzhou University

Nature Climate Change, 2013, vol. 3, issue 9, 822-826

Abstract: The El Niño/Southern Oscillation exhibits considerable natural variability on interdecadal to centennial timescales making it difficult to understand how climate change affects it. A reconstruction now shows there has been anomalously high activity in the late twentieth century, relative to the past seven centuries. This is suggestive of a response to global warming, and will provide constraints to improve climate models and projections.

Date: 2013
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DOI: 10.1038/nclimate1936

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