Nitryl chloride (ClNO2) is a dominant source of chlorine radical in polluted environment, and can significantly affect the atmospheric oxidative chemistry. However, the abundance of ClNO2and its exact role are not fully understood under different environmental conditions. During the summer of 2014, we deployed a chemical ionization mass spectrometer to measure ClNO2and dinitrogen pentoxide (N2O5) at a rural site in the polluted North China Plain. Elevated mixing ratios of ClNO2(>350pptv) were observed at most of the nights with low levels of N2O5(<200pptv). The highest ClNO2mixing ratio of 2070pptv (1min average) was observed in a plume from a megacity (Tianjin), and was characterized with a faster N2O5heterogeneous loss rate and ClNO2production rate compared to average conditions. The abundant ClNO2concentration kept increasing even after sunrise, and reached a peak 4h later. Such highly sustained ClNO2peaks after sunrise are discrepant from the previously observed typical diurnal pattern. Meteorological and chemical analysis shows that the sustained ClNO2morning peaks are caused by significant ClNO2production in the residual layer at night followed by downward mixing after breakup of the nocturnal inversion layer in the morning. We estimated that ∼ 1.7-4.0ppbv of ClNO2would exist in the residual layer in order to maintain the observed morning ClNO2peaks at the surface site. Observation-based box model analysis show that photolysis of ClNO2produced chlorine radical with a rate up to 1.12ppbvhĝ'1, accounting for 10-30% of primary ROxproduction in the morning hours. The perturbation in total radical production leads to an increase of integrated daytime net ozone production by 3% (4.3ppbv) on average, and with a larger increase of 13% (11ppbv) in megacity outflow that was characterized with higher ClNO2and a relatively lower oxygenated hydrocarbon (OVOC) to non-methane hydrocarbon (NMHC) ratio.