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The contribution of eastern-boundary density variations to the Atlantic meridional overturning circulation at 26.5 N

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Figure

Fig. 1.Distribution of the RAPID/MOCHA moorings across26.5◦ N as deployed for year 2007.
Table 2. Periods of mooring records and nominal pressure levels of sensors of EB1 mooring.
Fig. 3. 2-day low-pass filtered in-situ density anomaly at EB1, (a)from 0 to 2000 m and (b) from 2000 m to the bottom
Fig. 6. 2-day low-pass filtered temperature anomaly at EBH, (a)from 0 to 2000 m and (b) from 2000 m to the bottom
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