The Atlantic Ocean is Earth's second-largest ocean, covering approximately one_fifth of its surface. The ocean's name, derived from Greek mythology, means the "Sea of Atlas".
This ocean occupies an elongated, S-shaped basin extending in a north-south direction and is divided into the North Atlantic and South Atlantic by equatorial counter currents at about 8° north latitude. Bounded by North and South America on the west and Europe and Africa on the east, the Atlantic is linked to the Pacific Ocean by the Arctic Ocean on the north and the Drake Passage on the south. An artificial connection between the Atlantic and Pacific is also provided by the Svalbard to northern Ireland on a fair day.
Covering approximately 20% of Earth's surface, the Atlantic Ocean is second only to the Pacific in size. With its adjacent seas it occupies an area of about 41,100,000 square miles (106,400,000 km²) without them, it has an area of 31,800,000 mi³ (82,400,000 km²). The land area that drains into the Atlantic is four times that of either the Pacific or Indian oceans. The volume of the Atlantic Ocean with its adjacent seas is 354,700,000 km³ (85,100,000 mi³) and without them 323,600,000 km³ (77,640,000 mi³).
The average depth of the Atlantic, with its adjacent seas, is 3,332 m (10,932 ft); without them it is 3,926 m (12,881 ft). The greatest depth, 8,605 m (28,232 ft), is in the Puerto Rico Trench. The width of the Atlantic varies from 2,848 km (1,770 miles) between Brazil and Liberia to about 4,830 km (3,000 miles) between the United States and northern Africa.
The Atlantic Ocean has irregular coasts indented by numerous bays, gulfs, and seas. These include the Caribbean Sea, Gulf of Mexico, Gulf of St. Lawrence, Mediterranean Sea, Black Sea, North Sea, Baltic Sea, and Norwegian-Greenland Sea. Islands in the Atlantic Ocean include Greenland, Iceland, Rockall, Ireland, Fernando de Noronha, the Azores, the Madeira Islands, the Canaries, the Cape Verde Islands, Bermuda, the West Indies, St. Helena, Tristan da Cunha, the Falkland Islands, and South Georgia Island.
The principal feature of the bottom topography of the Atlantic Ocean is a great submarine mountain range called the Mid-Atlantic Ridge. It extends from Iceland in the north to approximately 58° south latitude, reaching a maximum width of about 1,600 km (1,000 miles). A great rift valley also extends along the ridge over most of its length. The depth of water over the ridge is less than 2,700 m (8,900 ft) in most places, and several mountain peaks rise above the water, forming islands. The South Atlantic Ocean has an additional submarine ridge, the Walvis Ridge.
The Mid-Atlantic Ridge separates the Atlantic Ocean into two large troughs with depths averaging between 12,000 and 18,000 ft (3,700 and 5,500 m). Transverse ridges running between the continents and the Mid-Atlantic Ridge divide the ocean floor into numerous basins. Some of the larger basins are the Guiana, North American, Cape Verde, and Canaries basins in the North Atlantic. The largest South Atlantic basins are the Angola, Cape, Argentina, and Brazil basins.
The deep ocean floor is thought to be fairly flat, although numerous seamounts and some guyots exist. Several deeps or trenches are also found on the ocean floor. The Puerto Rico Trench, in the North Atlantic, is the deepest. The Laurentian Abyss is found off the eastern coast of Canada. In the south Atlantic, the South Sandwich Trench reaches a depth of 8,428 m (27,651 ft). A third major trench, the Romanche Trench, is located near the equator and reaches a depth of about 24,455 ft (7,454 m). The shelves along the margins of the continents constitute about 11% of the bottom topography. In addition, a number of deep channels cut across the continental rise.
Ocean sediments are composed of terrigenous, pelagic, and authigenic material. Terrigenous deposits consist of sand, mud, and rock particles formed by erosion, weathering, and volcanic activity on land and then washed to sea. These materials are largely found on the continental shelves and are thickest off the mouths of large rivers or off desert coasts. Pelagic deposits, which contain the remains of organisms that sink to the ocean floor, include red clays and Globigerina, pteropod, and siliceous oozes. Covering most of the ocean floor and ranging in thickness from 60 m to 3,300 m (200 ft to 11,000 ft), they are thickest in the convergence belts and in the zones of upwelling. Authigenic deposits consist of such materials as manganese nodules. They occur where sedimentation proceeds slowly or where currents sort the deposits.
The salinity of the surface waters in the open ocean ranges from 33 to 37 parts per thousand by mass and varies with latitude and season. Although the minimum salinity values are found just north of the equator, in general the lowest values are in the high latitudes and along coasts where large rivers flow into the ocean. Maximum salinity values occur at about 25° north latitude. Surface salinity values are influenced by evaporation, precipitation, river inflow, and melting of sea ice.
Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from less than −2 °C to 29 °C (28 °F to 84 °F). Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by 7 °C to 8 °C (13 °F to 15 °F).
The Atlantic Ocean consists of four major water masses. The North and South Atlantic central waters constitute the surface waters. The sub-Antarctic intermediate water extends to depths of 1,000 m (3,300 ft). The North Atlantic deep water reaches depths of as much as 4,000 m (13,200 ft). The Antarctic bottom water occupies ocean basins at depths greater than 4,000 m (13,200 ft).
Due to the Coriolis force, water in the North Atlantic circulates in a clockwise direction, whereas water circulation in the South Atlantic is counter clockwise. The South tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur during each 24 lunar hours. The tides are a general wave that moves from south to north. In latitudes above 40° north some east-west oscillation occurs.
The climate of the Atlantic Ocean and adjacent land areas is influenced by the temperatures of the surface waters and water currents as well as the winds blowing across the waters. Because of the oceans' great capacity for retaining heat, maritime climates are moderate and free of extreme seasonal variations. Precipitation can be approximated from coastal weather data and air temperature from the water temperatures. The oceans are the major source of the atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest climatic zones stretch across the Atlantic north of the equator. The coldest zones are in the high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents contribute to climatic control by transporting warm and cold waters to other regions. Adjacent land areas are affected by the winds that are cooled or warmed when blowing over these currents. The Gulf Stream, for example, warms the atmosphere of the British Isles and northwestern Europe, and the cold water currents contribute to heavy fog off the coast of northeastern Canada (the Grand Banks area) and the northwestern coast of Africa. In general, winds tend to transport moisture and warm or cool air over land areas. Hurricanes develop in the southern part of the North Atlantic Ocean.
History and economy
The Atlantic Ocean appears to be the youngest of the world's oceans. Evidence indicates that it did not exist prior to 180 million years ago, when the continents that formed from the breakup of the ancestral supercontinent, Pangaea, were being rafted apart by the process of seafloor spreading. The Atlantic has been extensively explored since the earliest settlements were established along its shores. The Portuguese, and Christopher Columbus were the most famous among its early explorers. After Columbus, European exploration rapidly accelerated, and many new trade routes were established. As a result, the Atlantic became and remains the major artery between Europe and the Americas (known as transatlantic trade). Numerous scientific explorations have been undertaken, including those by the German Meteor expedition, Columbia University's Lamont Geological Observatory, and the U.S. Navy Hydrographic Office.
The ocean has also contributed significantly to the development and economy of the countries around it. Besides its major "transatlantic" transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves and the world's richest fishing resources, especially in the waters covering the shelves. The major species of fish caught are cod, haddock, hake, herring, and mackerel. The most productive areas include the Grand Banks off Newfoundland, the shelf area off Nova Scotia, Georges Bank off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Dogger bank of the North Sea, and the Falkland Banks. Eel, lobster, and whales have also been taken in great quantities. All these factors, taken together, tremendously enhance the Atlantic's great commercial value. Because of the threats to the ocean environment presented by oil spills, plastic debris, and the incineration of toxic wastes at sea, various international treaties exist to reduce some forms of pollution.
Location: body of water between Africa, Southern Ocean, and the Americas
Geographic coordinates: 0 00 N, 25 00 W
Map references: World
- total: 76.762 million km²
- note: includes Baltic Sea, Black Sea, Caribbean Sea, Davis Strait, Denmark Strait, part of the Drake Passage, Gulf of Mexico, Mediterranean Sea, North Sea, Norwegian Sea, almost all of the Scotia Sea, and other tributary water bodies
Area - comparative: slightly less than 6.5 times the size of the US
Coastline: 111,866 km
Climate: Tropical cyclones (hurricanes) develop anywhere from off the coast of Africa near Cape Verde to the Windward Islands and move westward into the Caribbean Sea or up the east coast of North America; hurricanes can occur from May to December, but are most frequent from late July to early November. Storms are common in the North Atlantic during northern winters, making ocean crossings more difficult and dangerous.
surface usually covered with sea ice in Labrador Sea, Denmark Strait, and Baltic Sea from October to June; clockwise warm-water gyre (broad, circular system of currents) in the northern Atlantic, counter-clockwise warm-water gyre in the southern Atlantic; the ocean floor is dominated by the Mid-Atlantic Ridge, a rugged north-south centerline for the entire Atlantic basin first discovered by the Challenger Expedition.
oil and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, precious stones
Icebergs common in Davis Strait, Denmark Strait, and the northwestern Atlantic Ocean from February to August and have been spotted as far south as Bermuda and the Madeira Islands; ships subject to superstructure icing in extreme northern Atlantic from October to May; persistent fog can be a maritime hazard from May to September; hurricanes north of the equator (May to December)
Environment – current issues
Endangered marine species include the manatee, seals, sea lions, turtles, and whales; drift net fishing is killing dolphins, albatrosses and other seabirds (petrels, auks), hastening the decline of fish stocks and contributing to international disputes; municipal sludge pollution off eastern US, southern Argentina; oil pollution in Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea; industrial waste and municipal sewage pollution in Baltic Sea, North Sea, and Mediterranean Sea
Geography – note
Major chokepoints include the Dardanelles, Strait of Gibraltar, access to the Panama and Suez Canals; strategic straits include the Strait of Dover, Straits of Florida, Mona Passage, The Sound (Oresund), and Windward Passage; the Equator divides the Atlantic Ocean into the North Atlantic Ocean and South Atlantic Ocean (previously known as the Ethiopic Ocean). During the Cold War the so called Greenland-UK (GIUK) Gap was a major strategic concern, the seabed in that area was laid with extensive hydrophone systems to track Soviet submarines.
Ports and harbours
Abidjan (Côte d'Ivoire), Accra (Ghana), Amsterdam (Netherlands), Antwerp (Belgium), Bahia Blanca (Argentina), Baltimore (US), The Gambia), UK), Norway), Bissau (Guinea-Bissau), Bordeaux (France), Boston (US), Germany), Brest (France), Bristol (UK), Buenos Aires (Argentina), Cadiz (Spain), Cape Town (South Africa), Casablanca (Morocco), Cayenne (French Guiana), Charleston (US), Cherbourg (France), Conakry (Guinea), Cork (Republic of Ireland), Cotonou (Benin), Dakar (Senegal), Douala (Cameroon), Republic of Ireland), Dunkirk (France), Edinburgh (UK), Fortaleza (Brazil), Georgetown (Guyana), Glasgow (UK), Germany), Canada), Jacksonville (US), La Coruña (Spain), Lagos (Nigeria), Las Palmas (Canary Islands, Spain), Le Havre (France), Libreville (Gabon), Lisbon (Portugal), Liverpool (UK), Lomé (Togo), UK), Angola), Malabo (Equatorial Guinea), Liberia), Uruguay), Canada), New Haven (US), New York (US), Newcastle upon Tyne (UK), Newport News (US), Norfolk (US), Nouakchott (Mauritania), Oslo (Norway), Belgium), Suriname), Philadelphia (US), Port Harcourt (Nigeria), Portugal), Benin), Portsmouth (UK), Portsmouth (US), Providence (US), Rabat (Morocco), Recife (Brazil), Rio de Janeiro (Brazil), Rotterdam (Netherlands), Brazil), Spain), Santos (Brazil), Savannah (US), Seville (Spain), Southampton (UK), Tangier (Morocco), Trondheim (Norway), Vigo (Spain), Walvis Bay (Namibia), Wilmington (US)
Transportation – note
Kiel Canal and Saint Lawrence Seaway are two important waterways