The
Antarctic Convergence is a curve continuously encircling
Antarctica where cold, northward-flowing Antarctic waters meet the relatively warmer waters of the
subantarctic. Antarctic waters predominantly sink beneath subantarctic waters, while associated zones of mixing and
upwelling create a zone very high in marine productivity, especially for
Antarctic krill. This line, like the
Arctic tree line, is a natural boundary rather than an artificial one like a line of latitude. It not only separates two
hydrological regions, but also separates areas of distinctive marine life associations and of different
climates. There is no
Arctic equivalent, due to the amount of land surrounding the northern polar region.