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Map of the strongest stratification found in the water column. Â Vertical mixing is easiest in regions where stratification is weak. Â The dependence on season is strongest in polar regions, especially regions associated with deep convection in the North Atlantic and the Southern Ocean.
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Depth of the pycnocline extracted from the MIMOCÂ http://www.pmel.noaa.gov/mimoc/ data set. Â You can see the seasonal oscillation between deep convection and shallow stratification in the polar regions. Â Also visible is the persistent pool of warm water in the West Pacific in contrast to the shallow stratification near the strong upwelling off the west coast of South America.
