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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 19, 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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- Upon its onset, its subsequent performance is notably influenced by sea-surface temperatures. The NEM rains are positively impacted during the prevalence of an active Indian-Ocean Dipole (IOD) phase (warmer sea surface temperatures in the western Indian Ocean) as well as the El Niño phase (warmer sea surface temperatures in the equatorial Pacific)....
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 …
Wikipedia · Text under CC-BY-SA license- Estimated Reading Time: 6 mins
The monsoon currents in the north Indian Ocean - ScienceDirect
WEBJan 1, 2002 · The monsoon currents are the seasonally reversing, open-ocean currents that flow between the Arabian Sea and the Bay of Bengal, the two wings of the north …
- Author: D. Shankar, P.N. Vinayachandran, A.S. Unnikrishnan
- Publish Year: 2002
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WEBDuring the northeast monsoon season, the country receives about 11% of its annual rainfall, while many districts over the south penin-sula receive 30–60% of their annual rainfall. …
WEBThe monsoon currents are the seasonally reversing, open-ocean currents that flow between. the Arabian Sea and the Bay of Bengal, the two wings of the north Indian …
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The monsoon currents in the north Indian Ocean | Request PDF
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