
A recurring pattern of climate system behavior that explains a significant portion of natural variability.A mode of variability is a recurring, organized pattern of change in a climate system that stands out from random fluctuations. Think of it as a 'favorite dance' the atmosphere and ocean perform together—not a single event, but a repeating rhythm that shifts temperatures, winds, and rainfall across large regions. These modes explain why some years are warmer or wetter than others in specific places, even when the overall global trend is steady.
The concept grew out of early 20th-century efforts to understand regional climate, with the discovery of the Southern Oscillation in the 1920s and the North Atlantic Oscillation in the 1930s. Statistical methods like empirical orthogonal functions, developed in the mid-20th century, formalized the identification of such modes.
Climate data, such as sea-surface temperatures or pressure fields, are analyzed statistically to find patterns that appear again and again. Each mode is characterized by a spatial pattern—where the anomalies are strong or weak—and a time series that shows when it is active. Physically, these modes arise from interactions between the ocean and atmosphere, such as how warm ocean water alters winds, which in turn change ocean currents, creating a feedback loop that sustains the pattern for months or years.
Modes of variability are used to make seasonal forecasts, since knowing the state of a mode like El Niño helps predict temperature and precipitation anomalies months ahead.
The El Niño–Southern Oscillation, the most famous mode of variability, shifts weather patterns across more than half the globe, from droughts in Australia to floods in South America.









