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The Oceanic Eddy Heat Transport

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Figure

Figure 1. Zonally integrated total time-mean northward heat transport (heavy line) and eddy rectified portion of the total (thinline) for (a) the World Ocean, (b) the Indian Ocean, (c) the Pacific Ocean and (d) the Atlantic Ocean.
Figure 3. Zonally integrated northward eddy heat transportbroken down by depth bin, for surface 25 m (heavy solidline), 25–985 m (dashed line), 985–2750 m (dashed-dottedline) and 2750–5200 m (light solid line).
Figure 4. Eddy transport decomposed by dynamical compo-nent, for the Ekman overturning (heavy solid line), the gyrecomponent (dashed line), the zonal mean shear (dashed-dotted line) and the eddy component (thin solid line).
Figure 6. (a) Instantaneous streamfunction and tempera-ture for jet with standing wave pattern in it
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