The Madden-Julian Oscillation (MJO) is a significant meteorological phenomenon characterized by the eastward movement of convection and weather patterns across tropical regions1. It is a type of atmospheric oscillation that occurs primarily during the Northern Hemisphere winter, with a quasi-periodic cycle ranging from approximately 30 to 90 days5. The MJO involves alternating phases of enhanced and suppressed convection, which are not fixed in duration, hence the term "quasi-periodic" oscillation5.
The MJO is a key source of predictability for extended-range forecasts, making it essential for predicting extreme weather events and short-term climate variations6. Improving MJO prediction capabilities is a priority for many research centers and operational forecasting units8. Recent advancements in model initialization, such as incorporating humidity data, have shown significant improvements in MJO forecasting skills10.
Studies have demonstrated that the MJO's impact on regional climate can be substantial, such as its influence on marine heatwaves in the southeastern tropical Indian Ocean7. Understanding the MJO's dynamics and its interactions with other climate phenomena is critical for enhancing climate models and improving forecast accuracy9.
In summary, the MJO is a vital component of the Earth's climate system, with far-reaching effects on tropical and global weather patterns. Ongoing research aims to deepen our understanding of the MJO to better predict and mitigate its impacts on weather and climate.