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Meridional transport of salt in the global ocean from an eddy-resolving model

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Figure

Fig. 1. Top panel: evaporation–precipitation–runoff flux for theglobal ORCA12 model (kgm−2 s−1)
Fig. 2. Box model used to introduce the salt transport decomposi-between the boxes at equilibrium
Fig. 4. Decomposition of the global meridional transport of salt inthe ORCA12 simulation
Fig. 5. Further analysis of the meridional transport of salt in thetwo components: the “overturning” (transport by the zonally aver-aged, depth-dependent velocity) and the “gyre” component
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