<p indent="0mm">Fine particulate matter (PM<sub>2.5</sub>) and ozone (O<sub>3</sub>) are currently the most concerning air pollutants. Long-term exposure to PM<sub>2.5</sub> and O<sub>3</sub> can induce cardiovascular diseases, presbyopia, and preterm birth. Acute exposure to PM<sub>2.5</sub> and O<sub>3</sub> can also result in hypertension and decreased heart rate variability. In recent years, PM<sub>2.5</sub> pollution abatement in China has achieved remarkable results, but O<sub>3</sub> pollution issues have emerged. In the troposphere, O<sub>3</sub> and PM<sub>2.5</sub> have a close association, i.e., O<sub>3</sub> can oxidize gaseous precursors to form sulfate, nitrate, ammonium and secondary organic aerosols in PM<sub>2.5</sub>, and PM<sub>2.5</sub> affects the generation and removal of O<sub>3</sub> by providing surfaces for heterogeneous reactions. Recent studies show that PM<sub>2.5</sub> and O<sub>3</sub> have a significant positive correlation in the photochemically active season in the Pearl River Delta (PRD) region. However, it is still difficult to achieve cooperative control for PM<sub>2.5</sub> and O<sub>3</sub> due to our limited knowledge of their coupling relationship. To date, most studies have focused on the photochemical mechanism in the daytime, and our understanding of the chemical processes at night is insufficient. As an important reactive intermediate, N<sub>2</sub>O<sub>5</sub> mainly accumulates through the nocturnal reaction of NO<sub>2</sub> and O<sub>3</sub> and is removed by heterogeneous reactions to produce HNO<sub>3</sub>. These processes directly affect ozone production and particulate matter formation. In addition to losing NO<sub><italic>x</italic></sub>, the heterogeneous reaction of N<sub>2</sub>O<sub>5</sub> would lead to particulate nitrate formation and photolabile species (i.e., ClNO<sub>2</sub>) release. ClNO<sub>2</sub> is a reservoir of NO<sub>2</sub> and chlorine, providing a connection between nitrogen oxide pollution and halogen activation. The formation of ClNO<sub>2</sub> represents an activation process of chlorine from the aerosol phase to the gas phase. ClNO<sub>2</sub> photolysis releases chlorine radicals and oxidizes VOCs, which could increase radical levels and promote ozone formation. Moreover, NO<sub>2</sub> released via ClNO<sub>2</sub> photolysis also promotes O<sub>3</sub> formation in the morning. In coastal areas, sufficient particle chlorine in aerosols might be driven by sea salt chloride interactions, which lead to the formation of ClNO<sub>2</sub>. Therefore, with high concentrations of nitrogen oxides, nighttime heterogeneous N<sub>2</sub>O<sub>5</sub> reactions would make a substantial contribution to PM<sub>2.5</sub> and O<sub>3</sub> in coastal regions. Although several studies have shown that heterogeneous N<sub>2</sub>O<sub>5</sub> reactions play an important role in the formation of PM<sub>2.5</sub> and O<sub>3</sub>, related observations in China are limited. In this study, N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> were measured in Shenzhen during the season with severe ozone pollution in October 2018. Iodine chemical ionization time-of-flight mass spectrometry (TOF-CIMS, Aerodyne Inc.) was used to measure N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub>. Based on collocated measurements of gas- and particle-phase pollutants, we quantitatively calculated the nighttime heterogeneous reactions and assessed their reactivities. The results show that the highest concentrations of N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> could be up to 1524 and 477 pptv <sc>(5 min</sc> average, 1 pptv = <sc>1 pptv=10<sup>–3</sup> mm<sup>3</sup>/m<sup>3</sup>)),</sc> respectively, and they were affected by precursors. The concentrations of N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> had pronounced peaks from sunset to sunrise. The nitrate formed via N<sub>2</sub>O<sub>5</sub> reactions at night contributed 24%−60% of the total nighttime nitrate particles. In particular, the concentration of ClNO<sub>2</sub> had a noticeable peak in the morning, and the photolysis of ClNO<sub>2</sub> generated Cl radicals, which quickly removed alkanes, and the maximum removal efficiency was 2−3 times higher than that of OH radicals. In addition, the diurnal variation in VOCs with different reactivities also implies that chlorine radicals participate in the VOC oxidation cycle in the morning. This reflects that Cl radical-induced oxidation reactions could promote the generation of ozone and secondary organic aerosols through the HO<sub><italic>x</italic></sub> radical cycle. Our study shows that active nighttime heterogeneous reactions can significantly promote the formation of PM<sub>2.5</sub> and O<sub>3</sub> in the coastal areas of the PRD region. Thus, it is urgent to call for more studies in the future to coordinate the control of PM<sub>2.5</sub> and O<sub>3</sub> in the PRD region.