Articles | Volume 13, issue 3
https://doi.org/10.5194/cp-13-231-2017
https://doi.org/10.5194/cp-13-231-2017
Research article
 | 
15 Mar 2017
Research article |  | 15 Mar 2017

Tropical forcing of increased Southern Ocean climate variability revealed by a 140-year subantarctic temperature reconstruction

Chris S. M. Turney, Christopher J. Fogwill, Jonathan G. Palmer, Erik van Sebille, Zoë Thomas, Matt McGlone, Sarah Richardson, Janet M. Wilmshurst, Pavla Fenwick, Violette Zunz, Hugues Goosse, Kerry-Jayne Wilson, Lionel Carter, Mathew Lipson, Richard T. Jones, Melanie Harsch, Graeme Clark, Ezequiel Marzinelli, Tracey Rogers, Eleanor Rainsley, Laura Ciasto, Stephanie Waterman, Elizabeth R. Thomas, and Martin Visbeck

Data sets

The tree ring measurements from Campbell Island International Tree-Ring Data Bank https://www.ncdc.noaa.gov/paleo-search/study/21591

The Campbell Island temperature reconstruction NOAA/World Data Center for Paleoclimatology https://www.ncdc.noaa.gov/paleo-search/study/21590

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Short summary
The Southern Ocean plays a fundamental role in global climate but suffers from a dearth of observational data. As the Australasian Antarctic Expedition 2013–2014 we have developed the first annually resolved temperature record using trees from subantarctic southwest Pacific (52–54˚S) to extend the climate record back to 1870. With modelling we show today's high climate variability became established in the ~1940s and likely driven by a Rossby wave response originating from the tropical Pacific.