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Towards closure of regional heat budgets in the North Atlantic using Argo floats and surface flux datasets

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Figure

Fig. 2. Ta shows a seasonal cycle of about 1◦C, whilst T−hshows little seasonal variation
Figure 2  Seasonal cycle of the upper 300 m (magenta) and T -300m  (cyan) for different 10 x 10
Figure 3 ◦ Seasonal cycle in absorbed net flux for NCEP (red) and NOC (blue) derived using
Fig. 4. Seasonal cycle in the heat storage of the upper 300 m (Wm  −2) for different 10◦×10◦ boxes in the North Atlantic
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