Indian Ocean

Body of water between Africa, the Southern Ocean, Asia, and Australia

20 00 S, 80 00 E

70.56 million sq km

Almost seven times the size of the US

66,526 km

Northeast monsoon (December to April), southwest monsoon (June to October); tropical cyclones occur during May/June and October/November in the northern Indian Ocean and January/February in the southern Indian Ocean

264 million cu km

19.8%

The counterclockwise Indian Ocean Gyre comprised of the southward flowing warm Agulhas and East Madagascar Currents in the west, the eastward flowing South Indian Current in the south, the northward flowing cold West Australian Current in the east, and the westward flowing South Equatorial Current in the north; a distinctive annual reversal of surface currents occurs in the northern Indian Ocean; low atmospheric pressure over southwest Asia from hot, rising, summer air results in the southwest monsoon and southwest-to-northeast winds and clockwise currents, while high pressure over northern Asia from cold, falling, winter air results in the northeast monsoon and northeast-to-southwest winds and counterclockwise currents

The following are examples of features on the continental shelf of the Indian Ocean (see Figure 2): Exmouth Plateau Indus Canyon The Swatch of No Ground/Ganges Canyon (Bay of Bengal) Sunda Shelf

The following are examples of features on the continental slope of the Indian Ocean (see Figure 2): Bengal Fan Indus Fan

The following are examples of features on the abyssal plains of the Indian Ocean (see Figure 2): Arabian Basin Crozet Basin Madagascar Basin Mid-Indian Basin Mozambique Basin Wharton Basin

The following are examples of mid-ocean ridges on the floor of the Indian Ocean (see Figure 2): Central Indian Ridge Davie Ridge Southeast Indian Ridge Southwest Indian Ridge

The following are examples of undersea terrain features on the floor of the Indian Ocean (see Figure 2): Andaman-Nicobar Ridge Chagos-Laccadive Ridge Kerguelen Plateau Madagascar Plateau Mascarene Plateau Mozambique Plateau Ninetyeast Ridge

The following are examples of ocean trenches on the floor of the Indian Ocean (see Figure 2): Java/Sunda Trench (deepest point in the Indian Ocean)

The following are examples of atolls in the Indian Ocean (see Figure 2): Bassas da India Chagos Archipelago/Diego Garcia Europa Island Juan de Nova Island Lakshadweep Islands Maldive Islands Seychelles

Sea level

Java Trench -7,192 m unnamed deep

-3,741 m

The ocean is divided into three zones based on depth and light level; sunlight entering the water may travel about 1,000 m into the oceans under the right conditions, but there is rarely any significant light below 200 m euphotic zone: the upper 200 m (656 ft) is also called "sunlight" zone; only a small amount of light penetrates beyond this depth dysphotic zone: between 200 m (656 ft) and 1,000 m (3,280 ft), and also called the twilight zone; the intensity of light rapidly dissipates as depth increases, and photosynthesis is no longer possible aphotic zone: below 1,000 m (3,280 ft) and also called the midnight zone; sunlight does not penetrate to these depths

Oil and gas fields, fish, shrimp, sand and gravel aggregates, placer deposits, polymetallic nodules

Occasional icebergs pose navigational hazard in southern reaches

Major chokepoints include Bab el Mandeb, Strait of Hormuz, Strait of Malacca, southern access to the Suez Canal, and the Lombok Strait

Marine pollution from ocean dumping, improper waste disposal, and oil spills; oil pollution in Arabian Sea, Persian Gulf, and Red Sea; threats to coral reefs; loss of biodiversity; endangered marine species

Northeast monsoon (December to April), southwest monsoon (June to October); tropical cyclones occur during May/June and October/November in the northern Indian Ocean and January/February in the southern Indian Ocean

The Indian Ocean fisheries are the third most important in the world, accounting for 15.5%, or 12,220,000 mt of the global catch in 2020; tuna, small pelagic fish, and shrimp are important species in these regions; the Food and Agriculture Organization delineated two fishing regions in the Indian Ocean: Eastern Indian Ocean region (Region 57) is the most important and the fifth-largest-producing region in the world with 8.4%, or 6,590,000 mt, of the global catch in 2020; the region encompasses the waters north of 55º South latitude and east of 80º East longitude, including the Bay of Bengal and Andaman Sea, with the major producers including India (2,362,481 mt), Indonesia (1,940,558 mt), Burma (1,114,777 mt), Bangladesh (877,837 mt), and Sri Lanka (373,369 mt); the principal catches include shad, skipjack tuna, mackerel, shrimp, and sardinellas Western Indian Ocean region (Region 51) is the world’s sixth-largest-producing region with more than 7.1% or 5,630,000 mt of the global catch in 2020; this region encompasses the waters north of 40º South latitude and west of 80º East longitude, including the western Indian Ocean, Arabian Sea, Persian Gulf, and Red Sea, as well as the waters along the east coast of Africa and Madagascar, the south coast of the Arabian Peninsula, and the west coast of India; major producers include India (2,207,125 mt), Oman (580,048 mt), Pakistan (341,730 mt), and Mozambique (274,791 mt); the principal catches include skipjack and yellowfin tuna, mackerel, sardines, shrimp, and cephalopods Regional fisheries bodies: Indian Ocean Tuna Commission, Commission for the Conservation of Southern Bluefin Tuna, Regional Commission for Fisheries (Persian Gulf/Gulf of Oman), Southeast Asia Fisheries Development Center, Southwest Indian Ocean Fisheries Commission, South Indian Ocean Fisheries Agreement

Named for the country of India, which makes up much of its northern border