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Subantarctic

Adapted from Wikipedia · Discoverer experience

A stunning astronaut view of Heard Island in the southern Indian Ocean, featuring volcanic peaks and glaciers from space.

The sub-Antarctic zone is a special area in the Southern Hemisphere, just north of Antarctica. It lies between about 46° and 60° south of the Equator. This region includes many islands in the southern parts of the Atlantic, Indian, and Pacific oceans, especially those north of the Antarctic Convergence.

The Antarctic region and its boundary, the Antarctic Convergence

These islands are important because they have unique plants and animals that are not found anywhere else in the world. The cold and windy climate makes life there challenging, but some tough plants, birds, and insects have managed to survive.

Glaciers found on these subantarctic islands are called subantarctic glaciers. Glaciers on the actual continent of Antarctica are known as Antarctic glaciers. Both types of glaciers are important for understanding how Earth's climate has changed over time.

Geography

The subantarctic region is found in the Southern Hemisphere, just north of Antarctica. It lies roughly between 46° and 60° south of the Equator. This area includes many islands in the southern parts of the Atlantic, Indian, and Pacific oceans, especially those located north of a special ocean area called the Antarctic Convergence.

Diagram of the major ocean currents, showing the Antarctic Circumpolar Current (ACC). In addition to the global thermohaline circulation, the ACC strongly influences regional and global climate.

The subantarctic region has special ocean fronts and currents that shape its climate and wildlife. The Antarctic Circumpolar Current is the most important current in the Southern Ocean, flowing completely around the Earth. It connects the Atlantic, Indian, and Pacific Oceans and carries a huge amount of water. These ocean patterns help control the climate and support many kinds of sea life.

Some islands in this area, like the Crozet Islands and the Kerguelen Islands, are considered subantarctic. Others, such as the Falkland Islands, have different climates and landscapes but are still close to the Antarctic Convergence. The region's islands often have tundra landscapes, though some have trees or grasslands.

NameOceanAdministered by
Antipodes IslandsPacific OceanNew Zealand
Auckland IslandsPacific OceanNew Zealand
Bounty IslandsPacific OceanNew Zealand
Bouvet Island (Bouvetøya)Atlantic OceanNorway
Campbell Island GroupPacific OceanNew Zealand
Crozet Islands (French: Îles Crozet or officially Archipel Crozet)Indian OceanFrance
Heard Island and McDonald Islands (HIMI)Indian OceanAustralia
Kerguelen IslandsIndian OceanFrance
Macquarie IslandPacific OceanAustralia
Prince Edward IslandsIndian OceanSouth Africa
South Georgia GroupAtlantic OceanUnited Kingdom
South Sandwich IslandsAtlantic OceanUnited Kingdom
Snares IslandsPacific OceanNew Zealand
Name of GlacierLength or (Width)Location
Abbotsmith Glacier4.8 kmHeard Island
Allison GlacierHeard Island
Austin GlacierSouth Georgia Group
Bary GlacierSouth Georgia Group
Baudissin Glacier(2.8 km)Heard Island
Bertrab Glacier"small"South Georgia Group
Bogen Glacier"small"South Georgia Group
Briggs GlacierSouth Georgia Group
Brøgger Glacier13 kmSouth Georgia Group
Brown GlacierHeard Island
Brunonia GlacierSouth Georgia Group
Buxton GlacierSouth Georgia Group
Challenger GlacierHeard Island
Christensen GlacierSouth Georgia Group
Christensen GlacierBouvet Island
Christophersen GlacierSouth Georgia Group
Clayton GlacierSouth Georgia Group
Compton GlacierHeard Island
Cook GlacierSouth Georgia Group
Crean Glacier6 kmSouth Georgia Group
Deacock GlacierHeard Island
Dead End GlacierSouth Georgia Group
Downes GlacierHeard Island
Ealey GlacierHeard Island
Eclipse GlacierSouth Georgia Group
Esmark GlacierSouth Georgia Group
Fiftyone GlacierHeard Island
Fortuna GlacierSouth Georgia Group
Geikie GlacierSouth Georgia Group
Gotley Glacier13.2 kmHeard Island
Graae Glacier3.2 kmSouth Georgia Group
Grace GlacierSouth Georgia Group
Hamberg GlacierSouth Georgia Group
Harker GlacierSouth Georgia Group
Harmer GlacierSouth Georgia Group
Heaney GlacierSouth Georgia Group
Helland GlacierSouth Georgia Group
Henningsen GlacierSouth Georgia Group
Herz GlacierSouth Georgia Group
Hindle Glacier10 kmSouth Georgia Group
Hodges GlacierSouth Georgia Group
Horntvedt GlacierBouvet Island
Jacka Glacier1.3 kmHeard Island
Jenkins GlacierSouth Georgia Group
Jewell GlacierSouth Georgia Group
Keilhau Glacier8 kmSouth Georgia Group
Kjerulf GlacierSouth Georgia Group
König GlacierSouth Georgia Group
Lancing GlacierSouth Georgia Group
Lewald GlacierSouth Georgia Group
Lied GlacierHeard Island
Lucas GlacierSouth Georgia Group
Lyell GlacierSouth Georgia Group
Mary Powell GlacierHeard Island
Morris GlacierSouth Georgia Group
Murray SnowfieldSouth Georgia Group
Nachtigal GlacierSouth Georgia Group
Neumayer Glacier13 kmSouth Georgia Group
Nordenskjöld Glacier"large"South Georgia Group
Novosilski Glacier13 kmSouth Georgia Group
Paget Glacier6 kmSouth Georgia Group
Peters GlacierSouth Georgia Group
Philippi GlacierSouth Georgia Group
Posadowsky GlacierBouvet Island
Price GlacierSouth Georgia Group
Purvis GlacierSouth Georgia Group
Quensel Glacier"small"South Georgia Group
Risting GlacierSouth Georgia Group
Ross Glacier10 kmSouth Georgia Group
Ryan GlacierSouth Georgia Group
Salomon GlacierSouth Georgia Group
Schmidt GlacierHeard Island
Schrader GlacierSouth Georgia Group
Spenceley GlacierSouth Georgia Group
Stephenson GlacierHeard Island
Storey GlacierSouth Georgia Group
Twitcher Glacier6 kmSouth Georgia Group
Tyrrell GlacierSouth Georgia Group
Vahsel GlacierHeard Island
Webb Glacier3.2 kmSouth Georgia Group
Weddell Glacier3.2 kmSouth Georgia Group
Wheeler Glacier3.2 kmSouth Georgia Group
Winston GlacierHeard Island

Climate

Impact of climate change on SAMW

The Subantarctic Mode Water and Antarctic Intermediate Water work together like a carbon sink, taking in atmospheric carbon dioxide and keeping it stored. If the temperature of Subantarctic Mode Water goes up because of climate change, it will be able to hold less carbon dioxide. Studies using computer models show that if the amount of carbon dioxide in the air grows to about 860 parts per million by 2100—which is about twice what it is today—the Subantarctic Mode Water will become less dense and salty. This change might mean that these waters take in and keep less carbon dioxide in the Southern Ocean.

Flora and fauna

Main pages: Category:Flora of subantarctic islands and Category:Fauna of subantarctic islands

The Antarctic realm and Antarctic Floristic Kingdom include most plants and animals found on subantarctic islands. Many plants and animals here are found only in this area.

Subantarctic island example

See also: Category:Flora of Heard Island and McDonald Islands and Category:Fauna of Heard Island and McDonald Islands

The land and plants and animals of Heard Island and McDonald Islands keep changing because of volcanic activity, strong winds and waves, and climate change. Since the mid-1980s, we have seen new lava flows on Heard Island. Satellite imagery shows that McDonald Island grew from about 1 to 2.5 square kilometers between 1994 and 2004 because of volcanic activity.

Because Earth is getting warmer, glaciers on these islands are melting back. This creates new places on land and in fresh water where plants and animals can live.

Heard Island has many colonies of penguins and petrels, and large groups of seals that live on land. Because there are so many sea birds and marine animals here, the area is very important for nature. The waters around the islands have many different sea creatures, including corals, sponges, barnacles and echinoderms. These waters also help young fish grow.

Retreat of subantarctic glaciers

See also: Retreat of glaciers since 1850 and Glacier mass balance

Retreat of San Rafael Glacier from 1990 to 2000. San Quintín Glacier is shown in the background

Glaciers around the world, especially in the Southern Hemisphere, are shrinking faster than ever. Scientists have studied many glaciers in places like South America, New Zealand, and Antarctica, and they all show signs of retreat.

Many glaciers near Antarctica are also shrinking. On islands like Kerguelen, Heard, South Georgia, and Bouvet, the amount of ice has been decreasing a lot.

Heard Island, a volcano covered in ice, shows clear signs of glacier retreat. Between 1947 and 2004, the ice on Brown Glacier shrank by about a third. The ice cliffs that once reached the ocean have disappeared, and glaciers have pulled back far inland. Scientists think this is because the world is getting warmer. Studies since 2000 show the ice is melting even faster now. The glaciers on Heard Island will likely keep shrinking as the climate continues to change.

Images

Map showing the pattern of ocean currents known as thermohaline circulation, which helps distribute oxygen deep in the ocean.
A stunning glacier view in the Beagle Channel, part of Alberto de Agostini National Park in southern Chile.
A satellite view of the Thatcher Peninsula in South Georgia, featuring mountains and bays.
A historical black-and-white photograph showing the Neumayer Glacier in South Georgia, captured in 1882.
An old photograph showing Schleinitz Glacier and a small observatory building from 1882
A stunning view of Nordenskjold Glacier in South Georgia, showcasing the icy landscape of this remote island.
A stunning view of planet Earth from space.
A marker indicating the geographic South Pole in Antarctica, a key location for scientific research and exploration.
An icon showing the Earth to illustrate the concept of climate change.

Related articles

This article is a child-friendly adaptation of the Wikipedia article on Subantarctic, available under CC BY-SA 4.0.

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