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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
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 …
- Estimated Reading Time: 4 mins
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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)....
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
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
WEB1 day ago · The analysis reveals that the occurrence of summer Monsoon Depressions (MDs) over the North Arabian Sea is doubling during 2001–2022 compared to the …
WEBDec 20, 2023 · While the spatio-temporal characteristics of Indian summer monsoon precipitation and its extreme spells have been extensively studied, the northeast …
WEBJun 1, 2012 · The northeast monsoon is dry, stable and has less vertical extent compared to the southwest monsoon. This season is also termed the retreating (northeast) monsoon season or the post-monsoon season in …
Journal of Geophysical Research: Atmospheres
WEB4 days ago · The MC region behaves as a bridge between the East Asian monsoon region and the Australian monsoon region along the north–south direction. The East Asian …
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 …
Monsoon - Wikipedia
WEBA monsoon ( / mɒnˈsuːn /) is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation [1] but is now used to describe seasonal changes …
The monsoon currents in the north Indian Ocean | Request PDF
WEBJan 31, 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 …
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WEBJun 26, 2024 · The variation in the Asian summer monsoon anticyclone (ASMA) has long been of interest due to its effects on the weather and climate, as well as the vertical …
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WEBThese height differences are caused by persistent monsoon winds, which blow steadily from one direction for months at a time. For example, in the North-East monsoon …
Bay of Bengal currents during the Northeast Monsoon
WEBAug 1, 1998 · The data identify several new features in the Bay of Bengal: a shelf-break coastal current in the northeast corner, an eddy and subsurface jet near the South …
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WEBNov 24, 2020 · (Express Photo: Nirmal Harindran, File) What is the Northeast monsoon, and why is it important? India receives rainfall during two seasons. About 75 per cent of …
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WEBApr 3, 2016 · North-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 …
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WEBFeb 13, 2024 · The northeast monsoon is limited to south India, bringing rain to Tamil Nadu, Puducherry, Karaikal, Yanam, Andhra Pradesh, Kerala, Mahe, and south interior …
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WEBPaso the average high temperature on August 1 is 95 deg, dropping to 92 deg by the end of the month. While July is usually the wettest month, August comes in a close second as …
Missouri primary elections results for Springfield, surrounding area
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WEBThe average total precipitation nationwide for this year’s monsoon period until July 27 was 472 millimeters (18.6 inches), 1.3 times higher than the 356.7 millimeters average from …
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WEBJan 3, 2022 · They can be cold, warm, and hot. Warm ocean currents originate near the equator and move towards the poles or higher latitudes while cold currents originate …
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