GG 140 - Lecture 23 - El Niño

Lecture 23 - El Niño


The El Niño/Southern Oscillation (ENSO) phenomenon is the primary mode of variability in the equatorial Pacific Ocean. It is composed of two extreme states, El Niño and La Niña. The oscillation between these states can be seen in measurements of sea surface temperature (SST), sea level pressure, thermocline depth, and easterly trade wind strength. Changes in SST and pressure lead to shifting of convective activity across the equatorial Pacific. Changes in the strength of the easterly trade winds lead to changes in the depth of the thermocline, which affect coastal upwelling offshore of South America. If upwelling is reduced, primary productivity is reduced. The effect of ENSO on convection and coastal upwelling makes it an important factor for both agriculture and fishing industries.



Essentials of Meteology, Ch. 14

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