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Letter
Nature Geoscience 1, 844–848 (1 December 2008) | doi:10.1038/ngeo352
Increased multidecadal variability of the North Atlantic Oscillation since 1781
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Abstract
The North Atlantic Oscillation is a meridional oscillation of atmospheric mass measured between Iceland and the A|[ccedil]|ores, which drives winter climate variability in eastern North|[nbsp]|America and Europe. A prolonged period of the positive phase during the 1990s led to the suggestion that anthropogenic warming was affecting the behaviour of the North Atlantic Oscillation.
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