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Southern Oscillation Index

Earth science
Also known as: SOI

Quick Summary

The Southern Oscillation Index (SOI) measures the atmospheric component of the El Niño/Southern Oscillation (ENSO) phenomenon. It tracks interannual fluctuations in atmospheric pressure across the tropical Indo-Pacific region.1

The SOI compares pressure differences between Australia/Indonesia and the eastern South Pacific. A negative SOI indicates high pressure in the west and low pressure in the east, often coinciding with El Niño conditions. Conversely, a positive SOI signifies low pressure in the west and high pressure in the east, considered the "high phase".12

These pressure shifts influence global weather patterns, affecting rainfall and temperatures. The Southern Oscillation was first identified by Gilbert Walker in the early 20th century as he sought to predict monsoon behavior.12

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