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The Antarctic Convergence or Antarctic Polar Front is a marine belt encircling Antarctica where cold, northward-flowing Antarctic waters meet the warmer waters of the sub-Antarctic. The line, which varies in latitude seasonally, separates the clockwise Antarctic circumpolar current from other oceans. Antarctic waters predominantly sink beneath the warmer subantarctic waters, while associated zones of mixing and upwelling create a zone very high in marine productivity, especially for Antarctic krill.
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