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The Indian Ocean gyre is composed of two major currents: the South Equatorial Current, and the West Australian Current. Normally moving counter-clockwise, in the winter the Indian Ocean gyre reverses direction due to the seasonal winds of the South Asian Monsoon. In the summer, the land is warmer than the ocean, so surface winds blow from the ...
Pages in category "Currents of the Indian Ocean" The following 15 pages are in this category, out of 15 total. This list may not reflect recent changes. A.
The Indian Monsoon Current refers to the seasonally varying ocean current regime found in the tropical regions of the northern Indian Ocean. During winter, the flow of the upper ocean is directed westward from near the Indonesian Archipelago to the Arabian Sea .
The rest of the monsoon current system is excluded for simplicity. The MZC, which feeds the Agulhas Current, is also not drawn. Based on plots from Sen Gupta et al. [1] The EACC and the Somali Current (SC) are the principal LLWBCs in the Indian Ocean. [6] The East Indian Coastal Current (EIC) is sometimes considered a LLWBC. [7]
The cold Benguela Current originates from upwelling of water from the cold depths of the Atlantic Ocean against the west coast of the continent. The two currents do not "meet" anywhere along the south coast of Africa. The Agulhas Current (/ ə ˈ ɡ ʌ l ə s /) is the western boundary current of the southwest Indian Ocean.
visualisation of ocean currents. The Mozambique Current is an ocean current in the Indian Ocean, usually defined as warm surface waters flowing south along the African east coast in the Mozambique Channel, between Mozambique and the island of Madagascar. The classical definition of the Mozambique Current is that it is a strong, steady, western ...
The Equatorial Counter Current is an eastward flowing, wind-driven current which extends to depths of 100–150 metres (330–490 ft) in the Atlantic, Indian, and Pacific Oceans. More often called the North Equatorial Countercurrent (NECC) , this current flows west-to-east at about 3-10°N in the Atlantic , Indian Ocean and Pacific basins ...
The East Madagascar Current has a controlling role in the western boundary current of the southwest Indian Ocean together with the Mozambique Current. The mean speed of the East Madagascar Current varies between 0.2–0–9 m/s (0.66–0.00–29.53 ft/s) with a peak in spring and the lowest point in summer. [ 1 ]
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