EL NIÑO / SOUTHERN OSCILLATION (ENSO)
ENSO (short for El Niño / Southern Oscillation) is a recurring weather pattern influenced by water temperatures in the central and eastern tropical Pacific Ocean. During neutral conditions, convection associated with rising branches of the Walker Circulation is found over the Maritime continent, northern South America, and eastern Africa. During ENSO events like El Niño and La Niña, this circulation gets either pushed or pulled around (El Niño) or sent into overdrive (La Niña) across the Pacific.
I originally created these diagrams for NOAA’s Climate Program Office and Climate.gov (now Climate.us) in 2014. They have since been republished widely in research, white papers, and online.

