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The hypersaline currents originating in the Ross Sea, Antarctica are an important start point for one part of this system. As the sea ice freezes, the salt molecules can no longer be accommodated in the ice crystals, and are excluded from the matrix. The South polar winds are dominantly away from the Pole because of their density - temperature properties, and the land gradient from the S pole.

This salt is then blown around, and eventually reaches the sea, where it increases the density.

The waters offshore of Antarctica are much enriched in minerals from the glacial gouging of the rock basement. As a fine flour, the entrained minerals are readily available.

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