1. Record‐Breaking Precipitation in Indonesia's Capital of Jakarta in Early January 2020 Linked to the Northerly Surge, Equatorial Waves, and MJO.
- Author
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Lubis, Sandro W., Hagos, Samson, Hermawan, Eddy, Respati, Muhamad R., Ridho, Ainur, Risyanto, Paski, Jaka A. I., Muhammad, Fadhlil R., Siswanto, Ratri, Dian Nur, Setiawan, Sonny, and Permana, Donaldi S.
- Subjects
MESOSCALE convective complexes ,RAINFALL ,STORM surges ,MADDEN-Julian oscillation ,PRECIPITATION forecasting ,WATER vapor - Abstract
A record‐breaking extreme rainfall event, the highest amount recorded since 1866, hit Indonesia's capital, Jakarta, in early January 2020. This torrential rainfall was mainly caused by the convergence of moisture‐rich air due to an unusual blocking of cross‐equatorial northerly surge over Northwest Java by the southerly winds induced by a cyclonic flow over the Indian Ocean. This condition caused a local increase in the amount of water vapor over Jakarta that eventually led to the formation of clouds and heavy precipitation. In addition, the concurrent occurrences of convectively active phases of equatorial waves (Kelvin, TD‐type, and eastward propagating inertia‐gravity waves) and Madden‐Julian Oscillation during the event also partly contributed to the enhanced local moisture over the region by increasing low‐level moisture flux convergence. Together, these large‐scale dynamical drivers provided a convective environment that fostered the development of a massive rain‐producing mesoscale convective system and, consequently, extreme rainfall over the region. Plain Language Summary: A record‐breaking heavy rainfall event, the highest in the 156‐year historical records, hit Indonesia's capital, Jakarta, in early January 2020. The flooding induced by extreme rainfall caused tremendous damage to infrastructure and had significant socioeconomic impacts. This study examines the atmospheric driving mechanisms underlying this extreme event. We found that heavy rains were triggered by an increase in humid air due to the blocking of the northerly surge over Northwest Java by the southerly winds. This condition created conditions for the development of deep convection and heavy rain over the region. In addition, the large‐scale moisture convergence induced by some types of equatorial waves and Madden‐Julian Oscillation during the event further enhanced local moisture and supported the development of convective cells and extreme rainfall. Deepening the understanding of the atmospheric mechanisms driving this event may provide valuable information for forecasting precipitation extremes over Jakarta in the future. Key Points: An exceptionally high daily rainfall accumulation of up to 377 mm caused severe flash floods in Jakarta in early January 2020The extreme rainfall was mainly caused by convergence of moisture‐rich air due to an unusual blocking of northerly surges by southerly windsThe occurrences of equatorial waves and Madden Julian oscillation partly contributed to the enhanced local moisture by increasing low‐level moisture convergence [ABSTRACT FROM AUTHOR]
- Published
- 2022
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