Overview
The Southern Ocean is the ocean surrounding the continent of Antarctica. It forms a continuous body of water around the Antarctic continent and connects the Atlantic, Pacific and Indian Oceans.
It is the southernmost of Earth's five recognised oceans and is characterised by extremely cold waters, powerful winds, large waves, extensive seasonal sea ice and one of the most important ocean currents on Earth.
Geography of the Southern Ocean
The Southern Ocean surrounds Antarctica and extends northward into the southern parts of the Atlantic, Pacific and Indian Ocean basins.
Unlike most of the world's oceans, the Southern Ocean is defined primarily by the circulation of water around Antarctica rather than by surrounding continental boundaries.
Major geographical features
- Antarctica
- Antarctic Peninsula
- Drake Passage
- Scotia Sea
- Ross Sea
- Weddell Sea
- Amundsen Sea
- Bellingshausen Sea
- Southern Atlantic Ocean
- Southern Pacific Ocean
- Southern Indian Ocean
Size and Depth
| Property | Approximate information |
|---|---|
| Area | Approximately 20 million km², depending on the boundary definition used |
| Location | Surrounding Antarctica |
| Hemisphere | Southern Hemisphere |
| Major latitude boundary | Often defined around 60° south |
| Deepest regions | Several deep ocean basins and trenches occur around Antarctica |
The exact area of the Southern Ocean varies according to the geographical definition used.
The Southern Ocean Seafloor
The seafloor beneath the Southern Ocean contains deep basins, submarine ridges, continental shelves, abyssal plains and trenches.
Important features include:
- South Sandwich Trench
- Scotia Arc
- Kerguelen Plateau
- Macquarie Ridge
- Pacific-Antarctic Ridge
- Southwest Indian Ridge
- Antarctic continental shelf
Major Seas of the Southern Ocean
| Sea | Location / significance |
|---|---|
| Weddell Sea | Located east of the Antarctic Peninsula and adjacent to the Atlantic sector of Antarctica. |
| Ross Sea | A large embayment of the Southern Ocean south of the Pacific Ocean. |
| Amundsen Sea | Located along the coast of West Antarctica. |
| Bellingshausen Sea | Located west of the Antarctic Peninsula. |
| Scotia Sea | Situated between South America, the Antarctic Peninsula and several Southern Ocean island groups. |
Antarctic Sea Ice
Sea ice is one of the most important physical characteristics of the Southern Ocean.
Unlike the Antarctic Ice Sheet, which is land-based, sea ice forms when seawater freezes and floats on the ocean surface.
Seasonal cycle
Antarctic sea ice generally reaches its greatest extent during the Southern Hemisphere winter and its smallest extent during late summer.
Icebergs
The Southern Ocean contains some of the world's largest icebergs.
Icebergs are pieces of freshwater ice that have broken away from glaciers or ice shelves in a process known as calving.
They can drift for hundreds or even thousands of kilometres before melting or becoming grounded.
Antarctic Ice Shelves
Ice shelves are floating extensions of the Antarctic Ice Sheet. They form where land-based glacial ice flows from Antarctica onto the ocean.
Major Antarctic ice shelves include:
- Ross Ice Shelf
- Ronne Ice Shelf
- Filchner Ice Shelf
- Amery Ice Shelf
- Larsen Ice Shelf
The Antarctic Circumpolar Current
The Antarctic Circumpolar Current, or ACC, is the dominant ocean current of the Southern Ocean.
It flows from west to east around Antarctica and is the only major ocean current that completely circles a continent.
The current is driven primarily by the powerful westerly winds of the Southern Ocean.
Westerly Winds
Strong westerly winds dominate much of the Southern Ocean.
These winds are especially persistent because there is a broad belt of ocean surrounding Antarctica without major continents interrupting the atmospheric circulation.
The region is consequently famous for strong winds and rough seas.
Ocean Circulation
The Southern Ocean is a major component of global ocean circulation.
Cold, dense Antarctic waters can sink into the deep ocean and contribute to the formation of deep and bottom waters.
These waters can subsequently spread through the world's ocean basins.
Climate of the Southern Ocean
The Southern Ocean has one of the harshest marine climates on Earth.
Major characteristics include:
- Very low temperatures
- Strong winds
- Large waves
- Frequent storms
- Seasonal sea ice
- Long periods of winter darkness
- Very long summer daylight
The Roaring Forties
The Roaring Forties are a belt of strong westerly winds found approximately between 40° and 50° south latitude.
These winds are particularly strong over the Southern Ocean because there are relatively few large landmasses to interrupt the flow.
The Furious Fifties
The Furious Fifties are a region of strong westerly winds farther south, roughly between 50° and 60° south latitude.
Winds and waves can be particularly severe in this region.
The Screaming Sixties
The Screaming Sixties refer to the powerful winds found around the higher southern latitudes near Antarctica.
Together, the Roaring Forties, Furious Fifties and Screaming Sixties illustrate the exceptionally energetic atmospheric environment of the Southern Ocean.
Wildlife of the Southern Ocean
The Southern Ocean supports a highly productive marine ecosystem.
Important animals include:
- Antarctic krill
- Penguins
- Seals
- Whales
- Albatrosses
- Petrels
- Fish
- Squid
Antarctic Krill
Antarctic krill are small crustaceans that form one of the foundations of the Southern Ocean food web.
Large quantities of krill provide food for whales, seals, penguins, fish and seabirds.
Penguins
Several species of penguin are associated with the Antarctic region and Southern Ocean.
Important species include:
- Emperor penguin
- Adélie penguin
- Chinstrap penguin
- Gentoo penguin
- King penguin
- Macaroni penguin
Emperor Penguins
Emperor penguins are the largest penguin species.
They are uniquely adapted to the Antarctic environment and breed during the Antarctic winter.
Their ability to survive extreme cold and prolonged darkness makes them one of the most remarkable animals of the Southern Ocean region.
Antarctic Seals
The Southern Ocean supports several species of seal.
- Weddell seal
- Leopard seal
- Crabeater seal
- Ross seal
- Southern elephant seal
- Antarctic fur seal
Whales of the Southern Ocean
The Southern Ocean is an important feeding area for many whale species.
- Blue whale
- Fin whale
- Humpback whale
- Minke whale
- Southern right whale
- Sperm whale
- Orca
Many whales migrate between Antarctic feeding grounds and warmer waters at lower latitudes.
Albatrosses and Seabirds
The Southern Ocean is one of the world's most important environments for seabirds.
Albatrosses are especially well adapted to the region. Their enormous wings allow them to travel great distances using dynamic soaring over the ocean.
Other important seabirds include petrels, skuas and shearwaters.
Marine Food Web
Phytoplankton form the foundation of much of the Southern Ocean marine food web.
Phytoplankton are consumed by zooplankton and krill. Krill are then eaten by fish, penguins, seals, seabirds and whales.
Phytoplankton → Krill → Fish / Penguins / Seals → Whales and other predators
The Southern Ocean and Antarctica
The Southern Ocean completely surrounds Antarctica and plays a major role in the physical and biological environment of the continent.
The ocean transports heat towards and away from Antarctica, interacts with floating ice shelves and provides habitat for Antarctic marine life.
Antarctica and the Global Climate System
Antarctica and the Southern Ocean form a closely coupled climate system.
The Antarctic Ice Sheet stores enormous quantities of frozen freshwater, while the Southern Ocean absorbs heat and carbon dioxide from the atmosphere.
Changes in either the ocean or the ice sheet can therefore have consequences for the global climate system.
Southern Ocean Carbon Cycle
The Southern Ocean is an important region for the exchange of carbon dioxide between the atmosphere and the ocean.
Marine organisms absorb carbon dioxide through photosynthesis, while physical processes transport carbon into deeper layers of the ocean.
This makes the Southern Ocean an important component of the global carbon cycle.
Exploration of the Southern Ocean
The Southern Ocean has been explored by navigators, explorers, scientists and Antarctic expeditions for centuries.
Important figures include:
- James Cook
- James Clark Ross
- Roald Amundsen
- Robert Falcon Scott
- Ernest Shackleton
James Cook
Captain James Cook made important voyages through the southern oceans during the eighteenth century.
His expeditions demonstrated that Antarctica was not a temperate southern continent easily accessible from lower latitudes and contributed substantially to geographical knowledge of the Southern Ocean.
James Clark Ross
James Clark Ross led major British Antarctic expeditions in the nineteenth century.
His expeditions investigated Antarctic waters and discovered important geographical features, including the Ross Sea and Ross Ice Shelf region.
Ernest Shackleton
Ernest Shackleton became one of the most famous explorers of the Antarctic region.
His Endurance expedition demonstrated the extraordinary difficulties of operating ships in the ice-covered Southern Ocean.
Modern Scientific Research
Modern research in the Southern Ocean uses research vessels, autonomous instruments, satellites, aircraft, underwater vehicles and oceanographic moorings.
Scientists investigate:
- Ocean circulation
- Sea-ice dynamics
- Climate change
- Ocean chemistry
- Marine biology
- Carbon cycling
- Antarctic ice shelves
- Deep ocean circulation
- Atmosphere-ocean interactions
Antarctic Circumpolar Current and Climate
The Antarctic Circumpolar Current is fundamental to the isolation of Antarctica from warmer subtropical waters.
By circulating around Antarctica, it provides an important barrier to the direct northward transport of warm surface waters.
It is therefore a major feature of the Southern Hemisphere climate system.
Environmental Change
The Southern Ocean is undergoing significant environmental change associated with global warming and other human influences.
Important environmental issues include:
- Changes in Antarctic sea ice
- Ocean warming
- Ocean acidification
- Changes in marine ecosystems
- Ice-shelf melting
- Changes in krill populations
- Fishing pressure
- Marine pollution
Ocean Warming
The Southern Ocean absorbs a substantial amount of the excess heat associated with anthropogenic global warming.
Changes in ocean temperature can affect sea ice, marine ecosystems and the stability of Antarctic ice shelves.
Ocean Acidification
Increasing concentrations of atmospheric carbon dioxide lead to increased absorption of carbon dioxide by seawater.
This process causes ocean acidification, which can affect organisms that form shells or skeletons from calcium carbonate.
Fishing in the Southern Ocean
Commercial and scientific fisheries operate in parts of the Southern Ocean.
Important species and resources include Antarctic toothfish, Patagonian toothfish and Antarctic krill.
International management is important because Southern Ocean ecosystems are highly interconnected.
Conservation
The Southern Ocean contains some of the most remote and relatively undisturbed marine ecosystems on Earth.
Conservation measures include marine protected areas, fishing regulations, scientific monitoring and international cooperation.
Southern Ocean and the Five Oceans
| Ocean | Principal region |
|---|---|
| Pacific Ocean | Between Asia/Oceania and the Americas |
| Atlantic Ocean | Between the Americas and Europe/Africa |
| Indian Ocean | Between Africa, Asia and Australia |
| Arctic Ocean | Around the North Pole |
| Southern Ocean | Around Antarctica |
Southern Ocean and the Other Oceans
The Southern Ocean is unusual because it connects three of the world's major ocean basins through the Antarctic Circumpolar Current.
Water can circulate between the Atlantic, Pacific and Indian Oceans through the Southern Ocean.
Southern Ocean Timeline
Millions of years ago
Continental movements progressively established the geography of Antarctica and the surrounding oceans.
Opening of the Drake Passage
The development of an ocean connection between South America and Antarctica allowed a circumpolar ocean circulation to develop.
18th century
European voyages substantially increased geographical knowledge of the southern oceans.
19th century
Antarctic exploration expanded through expeditions led by James Clark Ross and others.
20th century
Antarctic scientific research became increasingly international and systematic.
21st century
Satellites, autonomous instruments and advanced oceanographic models have transformed understanding of the Southern Ocean.
Quick Facts About the Southern Ocean
| Feature | Information |
|---|---|
| Name | Southern Ocean |
| Location | Surrounding Antarctica |
| Hemisphere | Southern Hemisphere |
| Common northern boundary | Approximately 60° S |
| Approximate area | About 20 million km² |
| Major current | Antarctic Circumpolar Current |
| Major seas | Weddell Sea, Ross Sea, Amundsen Sea, Bellingshausen Sea and Scotia Sea |
| Major wildlife | Krill, penguins, seals, whales and seabirds |
| Major environmental feature | Seasonal Antarctic sea ice |
| Major landmass | Antarctica |
| Climate significance | Major component of global ocean circulation and carbon cycling |
Conclusion
The Southern Ocean is one of the most important components of Earth's ocean system. Surrounding Antarctica, it links the Atlantic, Pacific and Indian Oceans and supports a remarkable polar ecosystem.
Its Antarctic Circumpolar Current, sea ice, deep-water formation and exchange of heat and carbon with the atmosphere give it an influence that extends far beyond the Southern Hemisphere.
The Southern Ocean is therefore important not only as a geographical feature surrounding Antarctica, but also as a fundamental part of Earth's climate system and global circulation of the oceans.