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• W2964501211 abstract "Alpine glaciers are sensitive indicators of changes in climate, and their ubiquity in mountainous regions make them valuable proxies for terrestrial climate reconstructions worldwide. However, the timing and extent of glacier change across the South American mid-latitudes through the Holocene are still poorly constrained relative to their counterparts in the Northern Hemisphere. Here we report a new 10Be surface exposure-based chronology of moraines recording a series of progressively less-extensive glacier advances of Glaciar Torre (Argentina, 49.3°S/73.0°W) since the Last Glacial Maximum, with expansions culminating at 17,600 ± 900, 13,500 ± 500, 9700 ± 400, 6900 ± 200, 6100 ± 300, 4500 ± 200, and 530 ± 60 yr BP. The declining magnitude of Holocene glacier expansions parallels a gradual rise in local summer insolation intensity during the Holocene, while individual advances occurred during inferred negative Southern Annular Mode (SAM)-like states at centennial to millennial timescales. These observations suggest that (i) summer insolation intensity modulated antiphased trends in glacier extent in the polar hemispheres during the Holocene, and that (ii) centennial-scale ‘SAM-like’ temperature and precipitation anomalies paced glacier fluctuations throughout Patagonia. Given the persistence of the inferred ’SAM-like’ anomalies throughout the Holocene, the modern measured trend towards positive SAM index conditions could mark the onset of a fundamental shift in the climate of the Southern Hemisphere midlatitudes that warrants consideration in projections of future climate." @default.
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• W2964501211 date "2019-09-01" @default.
• W2964501211 modified "2023-10-05" @default.
• W2964501211 title "Holocene glacier fluctuations in Patagonia are modulated by summer insolation intensity and paced by Southern Annular Mode-like variability" @default.
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• W2964501211 cites W1976926894 @default.
• W2964501211 cites W1977015134 @default.
• W2964501211 cites W1978239142 @default.
• W2964501211 cites W1982446286 @default.
• W2964501211 cites W1982729439 @default.
• W2964501211 cites W1988331452 @default.
• W2964501211 cites W1993256894 @default.
• W2964501211 cites W1994664019 @default.
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• W2964501211 cites W2001821874 @default.
• W2964501211 cites W2003308485 @default.
• W2964501211 cites W2005035365 @default.
• W2964501211 cites W2005785847 @default.
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• W2964501211 cites W2010560237 @default.
• W2964501211 cites W2010902902 @default.
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• W2964501211 cites W2019623172 @default.
• W2964501211 cites W2036600554 @default.
• W2964501211 cites W2039452414 @default.
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• W2964501211 cites W2064235548 @default.
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• W2964501211 doi "https://doi.org/10.1016/j.quascirev.2019.05.029" @default.
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