Inter-hemispheric temperature variability over the past millennium

Raphael Neukom (), Joëlle Gergis, David J. Karoly, Heinz Wanner, Mark Curran, Julie Elbert, Fidel González-Rouco, Braddock K. Linsley, Andrew D. Moy, Ignacio Mundo, Christoph C. Raible, Eric J. Steig, Tas van Ommen, Tessa Vance, Ricardo Villalba, Jens Zinke and David Frank
Additional contact information
Raphael Neukom: Oeschger Centre for Climate Change Research, University of Bern
Joëlle Gergis: School of Earth Sciences, University of Melbourne
David J. Karoly: School of Earth Sciences, University of Melbourne
Heinz Wanner: Oeschger Centre for Climate Change Research, University of Bern
Mark Curran: Kingston Tasmania 7050, Australia
Julie Elbert: Oeschger Centre for Climate Change Research, University of Bern
Fidel González-Rouco: Instituto de Geociencias (CSIC-UCM) Universidad Complutense de Madrid
Braddock K. Linsley: Lamont-Doherty Earth Observatory, Columbia University, Palisades New York 10964, USA
Andrew D. Moy: Kingston Tasmania 7050, Australia
Ignacio Mundo: Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET-Mendoza
Christoph C. Raible: Oeschger Centre for Climate Change Research, University of Bern
Eric J. Steig: University of Washington, Seattle Washington 98195, USA
Tas van Ommen: Kingston Tasmania 7050, Australia
Tessa Vance: Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart Tasmania 7000, Australia
Ricardo Villalba: Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET-Mendoza
Jens Zinke: School of Earth and Environment, University of Western Australia Oceans Institute, 35 Stirling Highway Crawley WA 6009, Australia
David Frank: Oeschger Centre for Climate Change Research, University of Bern

Nature Climate Change, 2014, vol. 4, issue 5, 362-367

Abstract: Palaeoclimate temperature records are dominated by Northern Hemisphere reconstructions. This study introduces a new Southern Hemisphere millennial temperature reconstruction from terrestrial and oceanic proxy records. This highlights the asynchronicity of temperature fluctuations across the two hemispheres, which should be taken into consideration in climate models and projections.

Date: 2014
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DOI: 10.1038/nclimate2174

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