La Niña

GC: n

S: UNICEF – (last access: 5 July 2016); (last access: 5 July 2016).

N: 1. Origin and Etymology of la niña: Spanish, the (female) child.
First Known Use: 1988.
2. An irregularly recurring upwelling of unusually cold water to the ocean surface along the western coast of South America that often occurs following an El Niño and that disrupts typical regional and global weather patterns especially in a manner opposite to that of El Niño.
3. La Niña is characterized by unusually cold ocean temperatures in the Equatorial Pacific, compared to El Niño, which is characterized by unusually warm ocean temperatures in the Equatorial Pacific. The graphic below shows the sea surface temperature in the equatorial Pacific (20ºN-20ºS, 100ºE-60ºW) from Indonesia on the left to central America on the right.
4. Strong La Niña conditions during December 1998 are shown in the top panel. The Eastern Pacific is cooler than usual, and unusually cool water extends farther westward than is usual (see the blue color extending further off-shore from South America along the equator).
Normal Equatorial Pacific Ocean surface temperatures (December 1993) are shown in the middle panel, including the usual cool water, called the ‘cold tongue’, in the Eastern Pacific (in blue, on the right of the plot) and the usual warm water, called the ‘warm pool’ in the Western Pacific (in red, on the left).
Strong El Niño conditions, in December 1997, are shown on the bottom panel, with warm water (red) extending all along the equator.
El Niño and La Niña are opposite phases of the El Niño-Southern Oscillation (ENSO) cycle, with La Niña sometimes referred to as the cold phase of ENSO and El Niño as the warm phase of ENSO.

S: 1 & 2. MW – (last access: 5 July 2016). 3 & 4. (last access: 5 July 2016).


CR: El Niño, meteorology.