Southern annular mode-like changes in southwestern Patagonia at centennial timescales over the last three millennia
Author
dc.contributor.author
Moreno Moncada, Patricio
Author
dc.contributor.author
Vilanova, I.
Author
dc.contributor.author
Villa Martínez, Rodrigo
Author
dc.contributor.author
Garreaud Salazar, René
Author
dc.contributor.author
Rojas, M.
Author
dc.contributor.author
De Pol-Holz, Ricardo
Admission date
dc.date.accessioned
2019-03-15T16:06:49Z
Available date
dc.date.available
2019-03-15T16:06:49Z
Publication date
dc.date.issued
2014
Cita de ítem
dc.identifier.citation
Nature Communications, Volumen 5,
Identifier
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20411723
Identifier
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10.1038/ncomms5375
Identifier
dc.identifier.uri
https://repositorio.uchile.cl/handle/2250/166212
Abstract
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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 CO 2 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 i