The 2024 Asian–Australian monsoon (AAM) year, defined as April 2024 to March 2025, was notable. Based on available data, a prolonged rainy season was observed in most parts of the AAM region, except for the Meiyu Region, which corresponds to the area affected by the second stage of the East Asian summer monsoon. The rainy season also featured elevated near-surface air temperatures, a boreal summer rainfall surplus of approximately 20% across South, East, and Mainland Southeast Asia, an austral summer rainfall deficit of approximately 30% in Northern Australia, and a surplus of approximately 30% in the Maritime Continent. During boreal winter, a strong East Asian winter monsoon circulation led to below-average precipitation along East Asia’s climatological rain belt, including South China and Japan, accompanied by above-average near-surface air temperatures. Meanwhile, the 2024 AAM exhibited notable subseasonal variability, with abrupt alternations between dry/drought and wet/flood conditions, as well as between warm and cold episodes over many regions. It was also characterized by widespread extreme events, including but not limited to heavy rainfall, heatwaves, cold surges, and tropical cyclones. Such AAM-associated variability and extremes exerted considerable social impacts and caused substantial economic losses, highlighting the ongoing challenges in understanding and predicting the AAM at regional scales and multiple timescales.

Circulation anomalies in one region sometimes cause circulation anomalies in other regions, and the correlation between such regional circulation anomalies is referred to as the atmospheric teleconnection. Chinese scientists have conducted extensive research on the atmospheric teleconnection patterns, particularly those related to the Asian–Pacific monsoon. This review first introduces the basic concepts and historical development of atmospheric teleconnections, and then presents an overview of the studies related to the Asian–Pacific monsoon in recent years, especially those on the subseasonal timescale. The paper systematically summarizes 26 teleconnection patterns, including their main features and associated pioneering works. Particular emphasis is placed on the East Asian–Pacific teleconnection pattern that propagates poleward along the low-level southwesterly monsoonal winds. The wave train-type teleconnection patterns propagating along the upper-level westerly jets are also briefly reviewed.