Jakarta, the capital megacity of Indonesia located in the northwest of Java Island, Indonesia (Figure 1a), experienced an extraordinary heavy rainfall event in early January 2020. The highest amount reached up to 377 mm (14.83 inches) per day, making it a record-breaking number in observations since 1866. This extreme rainfall subsequently triggered widespread disastrous flooding in Jakarta and its surroundings in the early morning of 1 January 2020, leading to catastrophic losses. It is estimated that at least 173,000 people were evacuated, 66 people died, more than 60% of the residential areas were submerged, and the economic loss reached over US$700 million (Berlinger & Yee, 2020;Nisa, 2020). Because of the high vulnerability of Jakarta to rainfall extremes, a better understanding of the physical processes of heavy rainfall is needed to establish a reliable extended-range flood forecast system for this region.Numerous studies have examined the effects of large-scale atmospheric circulation on precipitation extremes and major floods in Jakarta. For example, the major flooding event in February 2007 (the second highest record-breaking precipitation event) was attributed to an intense and persistent cross-equatorial northerly surge (CENS) that created an intensive low-level wind convergence and favorable dynamic conditions for the