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• W2078341181 endingPage "573" @default.
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• W2078341181 abstract "Monsoon Forcing Dansgaard/Oeschger (D/O) events—the sudden, millennial-scale periods of warmth that punctuate the cold climate of the Last Glacial period, and Heinrich events—cold intervals characterized by tremendous discharges of icebergs into the North Atlantic, have been observed at many locations in the Northern Hemisphere but not extensively in the Southern Hemisphere. Kanner et al. (p. 570 , published online 12 January; see the Perspective by Rodbell ) present a stable isotope record from the central Peruvian Andes, which represents a record of the South American Summer Monsoon from 50,000 to 16,000 years ago and which contains the signals of D/O and Heinrich events. The Southern Hemisphere monsoon displayed an antiphase relationship to Northern Hemisphere monsoon intensity at the millennial scale, and Antarctic millennial-scale climate fluctuations influenced the South American Summer Monsoon." @default.
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• W2078341181 date "2012-02-03" @default.
• W2078341181 modified "2023-10-01" @default.
• W2078341181 title "High-Latitude Forcing of the South American Summer Monsoon During the Last Glacial" @default.
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• W2078341181 doi "https://doi.org/10.1126/science.1213397" @default.
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