Author
Listed:
- Patricio I. Moreno
(Universidad de Chile, Las Palmeras 3425, Casilla 653
Institute of Ecology and Biodiversity, Universidad de Chile, Las Palmeras 3425, Casilla 653
Center for Climate Research and Resilience, Universidad de Chile, Blanco Encalada 2002)
- I. Vilanova
(CONICET-Museo Argentino de Ciencias Naturales Bernardino Rivadavia, Sección Palinología del Cuaternario, Av. Angel Gallardo 470)
- R. Villa-Martínez
(Institute of Ecology and Biodiversity, Universidad de Chile, Las Palmeras 3425, Casilla 653
Center for Climate Research and Resilience, Universidad de Chile, Blanco Encalada 2002
GAIA-Antártica, Universidad de Magallanes, Avenida Bulnes 01890)
- R. D. Garreaud
(Center for Climate Research and Resilience, Universidad de Chile, Blanco Encalada 2002
Universidad de Chile, Blanco Encalada 2002)
- M. Rojas
(Center for Climate Research and Resilience, Universidad de Chile, Blanco Encalada 2002
Universidad de Chile, Blanco Encalada 2002)
- R. De Pol-Holz
(Center for Climate Research and Resilience, Universidad de Chile, Blanco Encalada 2002
Universidad de Concepción, Barrio Universitario s/n)
Abstract
Late twentieth-century instrumental records reveal a persistent southward shift of the Southern Westerly Winds during austral summer and autumn associated with a positive trend of the Southern Annular Mode (SAM) and contemporaneous with glacial recession, steady increases in atmospheric temperatures and CO2 concentrations at a global scale. However, despite the clear importance of the SAM in the modern/future climate, very little is known regarding its behaviour during pre-Industrial times. Here we present a stratigraphic record from Lago Cipreses (51°S), southwestern Patagonia, that reveals recurrent ~200-year long dry/warm phases over the last three millennia, which we interpret as positive SAM-like states. These correspond in timing with the Industrial revolution, the Mediaeval Climate Anomaly, the Roman and Late Bronze Age Warm Periods and alternate with cold/wet multi-centennial phases in European palaeoclimate records. We conclude that SAM-like changes at centennial timescales in southwestern Patagonia represent in-phase interhemispheric coupling of palaeoclimate over the last 3,000 years through atmospheric teleconnections.
Suggested Citation
Patricio I. Moreno & I. Vilanova & R. Villa-Martínez & R. D. Garreaud & M. Rojas & R. De Pol-Holz, 2014.
"Southern Annular Mode-like changes in southwestern Patagonia at centennial timescales over the last three millennia,"
Nature Communications, Nature, vol. 5(1), pages 1-7, September.
Handle:
RePEc:nat:natcom:v:5:y:2014:i:1:d:10.1038_ncomms5375
DOI: 10.1038/ncomms5375
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