Madden–Julian oscillation

The Madden–Julian oscillation (MJO) is a large-scale pattern of tropical atmospheric variability marked by eastward-moving regions of enhanced and suppressed cloud and rainfall. Its active pattern typically circles the tropics in about 30–60 days, affecting weather on weekly-to-monthly timescales and modulating rainfall and other weather systems.

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28 October 2026
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This article was researched and drafted with AI assistance and checked by an automated review pass. It is not guaranteed to be accurate — verify important facts against the references below.

Pattern and timescale

The MJO is an intraseasonal fluctuation in tropical clouds, rainfall, winds and pressure. Its characteristic pattern includes an area of enhanced convection and rainfall alongside a region of suppressed convection; the paired pattern propagates eastward through the tropics. The Australian Bureau of Meteorology describes it as a pulse of cloud and rainfall near the equator that typically recurs every 30 to 60 days. Unlike the more persistent, largely stationary tropical Pacific pattern associated with El Niño and La Niña, the MJO moves, and more than one episode may occur in a season.

Phases and monitoring

Operational monitoring commonly divides the MJO's path into eight broad geographic phases around the equator. These phase labels describe the approximate location of the disturbance, not eight separate physical causes. One monitoring approach combines information about cloudiness and winds in the lower and upper atmosphere to estimate the pattern's location and strength. When the signal is weak, its phase and expected influence are less distinct. The MJO's effects also vary by season and region, so phase-based forecasts indicate shifts in probabilities rather than certainty about local weather.

Weather influences

By shifting tropical convection and circulation, the MJO can alter the likelihood or timing of rainfall and influence monsoon activity and tropical cyclone conditions. Its atmospheric effects can also extend beyond the tropics, where circulation changes may affect temperature, storms or precipitation. These are statistical influences, not guarantees that a particular event will occur: local conditions and other climate patterns also matter. Its week-to-week evolution makes the MJO useful in extended-range weather outlooks, between short-range forecasts and seasonal climate predictions.

Discovery and scientific understanding

Atmospheric scientists Roland Madden and Paul Julian identified the oscillation in the early 1970s while examining tropical wind and pressure records. Its broad observed behavior is well established, but the processes that initiate, sustain and move it are complex. Research reviews compare multiple theories, including mechanisms involving moisture, convection, atmospheric circulation and waves; no single simple explanation captures every observed feature.

Key facts

Typical cycle
The MJO's eastward-moving tropical pattern typically recurs every 30–60 days, although its strength and duration vary.
Main signature
It features shifting regions of enhanced and suppressed tropical cloudiness and rainfall.
Monitoring phases
The MJO is commonly tracked through eight geographic phases around the equator; phase indicates location, not a guaranteed local forecast.
Discovery
Roland Madden and Paul Julian documented the oscillation in the early 1970s from tropical wind and pressure observations.
Weather relevance
The MJO can modulate monsoons, tropical cyclone activity and weather beyond the tropics, with impacts dependent on region and season.

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References

  1. 1.
    What is the MJO, and why do we care?

    NOAA Climate.gov · other · reliability: unverified · retrieved 28 October 2026

    Supports: MJO's eastward-moving cloud, rainfall, wind and pressure pattern; typical 30–60-day recurrence; phases, historical identification and weather impacts.

  2. 2.
    Madden-Julian Oscillation (MJO) monitoring

    Australian Bureau of Meteorology · other · reliability: unverified · retrieved 28 October 2026

    Supports: Definition, timescale, eight-phase monitoring approach and interpretation of MJO strength and location.

  3. 3.
    Four theories of the Madden-Julian Oscillation

    NOAA Pacific Marine Environmental Laboratory · other · reliability: unverified · retrieved 28 October 2026

    Supports: Overview of competing scientific theories and common emphases on convection, moisture and circulation in MJO dynamics.

  4. 4.
    Madden–Julian Oscillation: Bridging Weather and Climate

    Bulletin of the American Meteorological Society · other · reliability: unverified · retrieved 28 October 2026

    Supports: Peer-reviewed review of the MJO's relationships to weather and climate phenomena.

References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.

Article history

  1. Version 128 October 2026 · EditorCreated by Zapia