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Mechanisms of Atlantic Meridional Overturning Circulation variability simulated by the NEMO model

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Figure

Figure 1. Time series of annual mean AMOC-Ek variability forthe 4 model runs studied in this paper before they are linearly de-trended and deseasoned
Figure 2. Correlations of the annual AMOC-Ek at 26.5◦ N with the 1000–3000 m (a, c) and the top 1000 m (b, d) averaged density anomaliesin ORCA1-R07 (a, b) and ORCA025-G70 (c, d) runs, for the 45-year period 1960–2004 inclusive
Fig. 2g, h, and so we take this to be the signal of fast bound-ary waves similar to the HadCM3 results in Hermanson etal
Figure 4. Annual time series of AMOC-Ek transport anomalyable, shorter names R07 and G70 for legend have been used for theat 26.5◦ N (red) and density anomaly (blue) averaged over theLabrador and Irminger seas (between 50–35◦ W and 45–60◦ N) in1000–3000 m
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