La Niña: Sea Surface Temperature and Height Anomalies

  • Released Friday, February 7, 2014

The animation illustrates the evolution of sea surface temperature (SST) and sea surface height (SSH) anomalies (relative to the respective normal state) associated with the 2010-11 La Niña in the Pacific Ocean. SST and SSH anomalies reflect the heat content in the mixed layer (approximately upper 50 m) and the upper ocean (approximately upper 150 m) respectively. Warm/cold SST anomalies often are associated with high/low SSH anomalies. They provide complimentary views of the oceanic signature of climate variability such as El Niño and La Niña . La Niña is the cooling phase of an interannual mode of climate variability called El Niño-Southern Oscillation. Initial cooling appeared in the eastern to central equatorial Pacific around June 2010 and grew into a relatively strong La Niña event in late 2010. The event persists beyond February 2011.


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This page was originally published on Friday, February 7, 2014.
This page was last updated on Tuesday, November 14, 2023 at 12:25 AM EST.