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La Niña
[ lah nee-nyah ]
noun
- a cool ocean current that develops off the coast of Ecuador and Peru, sometimes following an El Niño but causing nearly the opposite extreme weather conditions.
La Niña
/ læ ˈniːnjə /
noun
- meteorol a cooling of the eastern tropical Pacific, occurring in certain years
La Niña
/ länēn′yä /
- A cooling of the surface water of the eastern and central Pacific Ocean, occurring somewhat less frequently than El Niño events but causing similar, generally opposite disruptions to global weather patterns. La Niña conditions occur when the Pacific trade winds blow more strongly than usual, pushing the sun-warmed surface water farther west and increasing the upwelling of cold water in the eastern regions. Together with the atmospheric effects of the related southern oscillation , the cooler water brings drought to western South America and heavy rains to eastern Australia and Indonesia.
- Compare El Niño
Word History and Origins
Origin of La Niña1
Word History and Origins
Origin of La Niña1
Example Sentences
One of the only long-term predictive measures that forecasters can use, the El Niño-Southern Oscillation cycle, or ENSO, remains in neutral, meaning that the Pacific Ocean isn’t currently in either a La Niña or El Niño cycle.
La Niña years typically favor drier conditions for the southwestern U.S.
La Niña seasons typically produce large numbers of atmospheric rivers, or narrow bands of concentrated water vapor in the sky that act like rivers in the sky.
This particular storm was exacerbated by the fact that it occurred as we enter the La Niña cycle, or a period in the ocean’s natural cycles when temperatures cool in the central and east-central equatorial Pacific region.
Many scientists expect the opposite, cooler phase, La Niña, to develop soon.
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