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Diapycnal oxygen supply to the tropical North Atlantic oxygen minimum zone

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Figure

Fig. 2. Vertical position of the deep oxygen minimum core in depthcoordinates (black isolines, metres) and in potential density coordi-nates (red isolines, kg m−3)
Fig. 3. Minimum covered area of tracer patch after 30 months (ma-genta filled contour) as well as locations of microstructure mea-surements (black squares) and stations with shear data from 75 kHzvessel-mounted ADCP (blue squares) during cruises in the peri
Fig. 4. Profiles of oxygen concentration, diapycnal diffusivity Kfrom microstructure measurements, and potential density, averagedacross the entire chosen analysis region of the OMZ
Fig. 5. Difference between the lateral average of local diapycnalfluxes and the product of laterally averaged diapycnal diffusivityand laterally averaged oxygen gradient as a function of depth
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