Guinea Current

Last updated
The South Atlantic Gyre. South Atlantic Gyre.png
The South Atlantic Gyre.

The Guinea Current is a slow warm water current that flows to the east along the Guinea coast of West Africa. It has some similarity to the Equatorial Counter Current in the Indian and Pacific Oceans.

See also


Related Research Articles

Geography of Guinea

Guinea is a country on the coast of West Africa and is bordered by Guinea-Bissau, Senegal, Mali, Ivory Coast, Liberia, and Sierra Leone.

Geography of Guinea-Bissau

The geography of Guinea-Bissau is that of low coastal plains bordering the Atlantic Ocean. The country borders Senegal in the north and Guinea in the southeast.

Island Any piece of sub-continental land that is surrounded by water

An island or isle is any piece of subcontinental land that is surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago.

Pacific Ocean Ocean between Asia and Australia in the west, the Americas in the east and Antarctica or the Southern Ocean in the south.

The Pacific Ocean is the largest and deepest of Earth's oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean in the south and is bounded by the continents of Asia and Australia in the west and the Americas in the east.

Gulf of Guinea The northeasternmost part of the tropical Atlantic Ocean from Cape Lopez in Gabon, north and west to Cape Palmas in Liberia

The Gulf of Guinea is the northeasternmost part of the tropical Atlantic Ocean from Cape Lopez in Gabon, north and west to Cape Palmas in Liberia. The intersection of the Equator and Prime Meridian is in the gulf.

Ocean current Directional mass flow of oceanic water generated by external or internal forces

An ocean current is a continuous, directed movement of sea water generated by a number of forces acting upon the water, including wind, the Coriolis effect, breaking waves, cabbeling, and temperature and salinity differences. Depth contours, shoreline configurations, and interactions with other currents influence a current's direction and strength. Ocean currents are primarily horizontal water movements.

Apostolic nunciature

An apostolic nunciature is a top-level diplomatic mission of the Holy See, equivalent to an embassy. However, it does not issue visas, nor does it have consulates.

Bismarck Sea Marginal sea in the southwestern Pacific Ocean northeast of the island of New Guinea and south of the Bismarck Archipelago and the Admiralty Islands

The Bismarck Sea lies in the southwestern Pacific Ocean within the nation of Papua New Guinea. It is located northeast of the island of New Guinea and south of the Bismarck Archipelago. It has coastlines in districts of the Islands Region, Momase Region, and Papua Region.

Organisation of African, Caribbean and Pacific States Intergovernmental organization of countries in Africa, the Caribbean, and the Pacific

The Organisation of African, Caribbean and Pacific States (OACPS) is a group of countries in Africa, the Caribbean, and the Pacific that was created by the Georgetown Agreement in 1975. Formerly known as African, Caribbean and Pacific Group of States (ACP), the organisation's main objectives are sustainable development and poverty reduction within its member states, as well as their greater integration into the world's economy. All of the member states, except Cuba, are signatories to the Cotonou Agreement with the European Union.

Oceanic languages Subgroup of the Austronesian language family

The approximately 450 Oceanic languages are a branch of the Austronesian languages. The area occupied by speakers of these languages includes Polynesia, as well as much of Melanesia and Micronesia. Though covering a vast area, Oceanic languages are spoken by only two million people. The largest individual Oceanic languages are Eastern Fijian with over 600,000 speakers, and Samoan with an estimated 400,000 speakers. The Gilbertese (Kiribati), Tongan, Tahitian, Māori, Western Fijian and Tolai languages each have over 100,000 speakers. The common ancestor which is reconstructed for this group of languages is called Proto-Oceanic.

Central–Eastern Malayo-Polynesian languages Proposed subgroup of the Austronesian language family

The Central–Eastern Malayo-Polynesian (CEMP) languages form a proposed branch of the Malayo-Polynesian languages consisting of over 700 languages.

Solomon Sea A sea in the Pacific Ocean between Papua New Guinea and the Solomon Islands

The Solomon Sea is a sea located within the Pacific Ocean. It lies between Papua New Guinea and the Solomon Islands. Many major battles were fought there during World War II.

Angola current is a temporary ocean surface current. It is an extension of the Guinea Current, flowing near western Africa's coast. It is known to have created similar effects in the upwelling as El Niño, though its effect is weaker.

Kokopo Place in East New Britain, Papua New Guinea

Kokopo is the capital of East New Britain in Papua New Guinea. It is administered under Kokopo-Vunamami Urban LLG.

Andrew Kenneth Pawley, FRSNZ, FAHA, is Emeritus Professor at the School of Culture, History & Language of the College of Asia & the Pacific at the Australian National University. Pawley was born in Sydney but moved to New Zealand at the age of 12.

Proto-Oceanic is a proto-language that historical linguists since Otto Dempwolff have reconstructed as the hypothetical common ancestor of the Oceanic subgroup of the Austronesian language family. Proto-Oceanic is a descendant of the Proto-Austronesian language (PAN), the common ancestor of the Austronesian languages.

The Lomonosov current is a deep current in the Atlantic Ocean.