Exploration of complex physical and chemical processes of a severe haze episode over central Taiwan

Abstract

Nitrate is one of the significant inorganic aerosols and is frequently experienced as the dominant component during air quality events in central Taiwan. This study examined a haze event with unprecedented PM_2.5 levels and peaked at 110 μg/m³ in central Taiwan's urban areas (UAPRS station) during 04–05 November 2021. Data showed PM_2.5 at UAPRS was 29.0 μg/m³ during the day and 89.7 μg/m³ at night. Notably, nitrate dramatically increased from 4.4 to 39.0 μg/m³, contributing 43.5 % to the nighttime rise in PM_2.5 in central Taiwan on the event day.

Simulation results indicated that the lee-side vortex, driven by the interaction between the ambient flow and the Central Mountain Range (CMR), facilitated the accumulation of pollutants, transporting them northward to the ocean and then returning as the ambient wind direction changed from easterly to southeasterly. Additionally, the swept-back plume in the afternoon, driven by the lee-side northwesterly flow and overlaid with urban pollution, was a key contributor to the first PM_2.5 peak at 20:00–22:00 LST on November 4. The mechanisms study revealed that nitrate aerosol was dominant, with N₂O₅ hydrolysis playing a critical role in its formation in the nocturnal atmospheric chemistry. Furthermore, the convergence of the lee-side northwesterly flow with the mountain downslope wind at midnight, combined with the reduction in planetary boundary layer height, enhanced the second PM_2.5 peak, which occurred between 02:00 and 03:00 LST on November 5. The findings of this study can be applied to other regions with similar complex topography, pollution environments, and comparable relief.