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Projection of North Atlantic Oscillation and its effect on tracer transport

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Academic year: 2017

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Figure 1. Leading empirical orthogonal function (EOF1) of the winter (DJF) mean sea-level pressure (SLP) anomalies in the North Atlantic sector (20–80 ◦ N, 90 ◦ W–40 ◦ E) of the coupled simulation considering the full period 1950–2100 (top), recent past pe
Figure 2. Normalized principal component time series (PC1) of the leading empirical orthogonal function (EOF1) of the winter mean sea-level pressure (SLP) anomalies for the entire simulation period (1950–2100)
Figure 4. NAO phase number distributions, computed in the recent past (left) and future (right) periods.
Figure 6. Differences between future (2070–2100) and recent past (1980–2010) temporal averages of CO_25 winter surface mixing ratio, both in the case of high NAO (PC1 > 0.5) (left) and low NAO (PC1 < −0.5) (right)
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