La Nina effect
![](https://civils360.com/wp-content/uploads/2022/01/La-Nina-effect-.jpg)
What is La Nina effect ?
La Nina, the “cool phase” of ENSO, is a pattern that describes the unusual cooling of the tropical eastern Pacific. La Nina events may last between one and three years, unlike El Nino, which usually lasts no more than a year. Both phenomena tend to peak during the Northern Hemisphere winter.
La Nina means The Little Girl in Spanish. It is also sometimes called El Viejo, anti-El Nino, or simply “a cold event.”
La Nina events represent periods of below-average sea surface temperatures across the east-central Equatorial Pacific.
It is indicated by sea-surface temperature decreased by more than 0.9℉ for at least five successive three-month seasons.
The La Nina event is observed when the water temperature in the Eastern Pacific gets comparatively colder than normal, as a consequence of which, there is a strong high pressure over the eastern equatorial Pacific.
La Nina is caused by a build-up of cooler-than-normal waters in the tropical Pacific, the area of the Pacific Ocean between the Tropic of Cancer and the Tropic of Capricorn.
La Nina is characterized by lower-than-normal air pressure over the western Pacific. These low-pressure zones contribute to increased rainfall.
La Nina events are also associated with rainier-than-normal conditions over southeastern Africa and northern Brazil.
However, strong La Nina events are associated with catastrophic floods in northern Australia.
La Nina is also characterized by higher-than-normal pressure over the central and eastern Pacific.
This results in decreased cloud production and rainfall in that region.
Drier-than-normal conditions are observed along the west coast of tropical South America, the Gulf Coast of the United States, and the pampas region of southern South America.
![](https://civilscopy.adsomia.in/wp-content/uploads/2022/01/La-Nina-effect.jpg)
La Nina influences the Indian subcontinent by piping in cold air from Siberia and South China, which interacts with the tropical heating to produce a north-south low-pressure system.
The cold air of La Nina associated with this north-south trough tends to extend much further south into India.
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