Antarctic Convergence

The Antarctic Convergence, better known as the Antarctic Polar Frontal Zone (or "Polar Front" for short), is a line encircling Antarctica where cold, northward-flowing Antarctic waters meet and mix with the relatively warmer waters of the sub-Antarctic. Antarctic waters predominantly sink beneath sub-Antarctic waters, while associated zones of mixing and upwelling create a zone very high in marine productivity, especially for Antarctic Krill. The line is actually a zone approximately convert|32|to|48|km|mi|abbr=on|lk=off wide, varying somewhat in latitude seasonally and in different longitudes, extending across the Atlantic, Pacific, and Indian Oceans between the 48th and 61st parallels of south latitude. The precise location at any given place and time is made evident by the sudden drop in temperature from north to south of, on average, 2.8 °C (37 °F) to 5.5 °C (42 °F), to below convert|2|°C|°F|abbr=on|lk=off. Although this zone is a mobile one, it usually does not stray more than a half a degree of latitude from its mean position.

There is no Arctic equivalent, due to the amount of land surrounding the northern polar region.

This line, like the Arctic tree line, is a natural boundary rather than one derived from reasoning. It not only separates two hydrological regions, but also separates areas of distinctive marine life associations and of different climates.

The South Shetland Islands, South Orkney Islands, South Georgia and the South Sandwich Islands, Bouvet Island, Heard Island and McDonald Islands all lie south of the Antarctic Convergence.

The Kerguelen Islands lie approximately on the Convergence; the Falkland Islands, Prince Edward Islands, Crozet Islands, Île Amsterdam, Île Saint-Paul, Tierra del Fuego and Macquarie Island lie north of the Convergence.

External links

* [http://carto.eu.org/article2436.html Map of Antarctic Convergence]

ee also

* Antarctic Circle
* Antarctic Circumpolar Wave
* Subantarctic