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- The Northeast Monsoon Current is a westward current that flows southwest and west, crossing the Equator during the northeast monsoon (November–March)12. It is strongest in February when it reaches 50 cm s −12. The current flows to the south of 5°N latitude3. Between the Northeast Monsoon Current and the westerly current maintained south of the Equator by the southeast trade winds, a strong Equatorial Countercurrent flows east at about latitude 10° S1.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.
During the northeast monsoon (November–March), the Indian North Equatorial Current (or Northeast Monsoon Drift) flows southwest and west, crossing the Equator. Between this westerly current and the westerly current maintained south of the Equator by the southeast trade winds, a strong Equatorial Countercurrent flows east at about latitude 10° S.
www.britannica.com/place/Monsoon-CurrentThe Northeast Monsoon Current is westward only during the months of January through March, and is strongest in February when it reaches 50 cm s −1. Estimates of westward volume transport range from 7 to 14 Sverdrups.
en.wikipedia.org/wiki/Indian_Monsoon_CurrentNorth-east monsoon winds blow from land to the ocean during winter season in the northern hemisphere and thus westward blowing north-east monsoon currents are produced between Andman and Somali (fig. 29.4). This current flows to the south of 5°N latitude.www.geographynotes.com/oceans/indian-ocean/6-… - People also ask
Monsoon Current | Map, Direction, & Facts | Britannica
WEBJul 20, 1998 · During the northeast monsoon (November–March), the Indian North Equatorial Current (or Northeast Monsoon Drift) flows southwest and west, crossing the Equator. Between this westerly current and the westerly current maintained south of …
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Indian Monsoon Current - Wikipedia
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. During the summer, the direction reverses, with eastward flow extending from Somalia into the Bay of Bengal. These variations …
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