Abstract. Co-occurrences of high concentrations of PM2.5 and ozone (O3) have
been frequently observed in haze-aggravating processes in the North China
Plain (NCP) over the past few years. Higher O3 concentrations on hazy
days were hypothesized to be related to nitrous acid (HONO), but the key sources
of HONO enhancing O3 during haze-aggravating processes remain unclear.
We added six potential HONO sources, i.e., four ground-based (traffic, soil,
and indoor emissions, and the NO2 heterogeneous reaction on ground
surface (Hetground)) sources, and two aerosol-related (the NO2
heterogeneous reaction on aerosol surfaces (Hetaerosol) and nitrate
photolysis (Photnitrate)) sources into the WRF-Chem model and designed
23 simulation scenarios to explore the unclear key sources. The results
indicate that ground-based HONO sources producing HONO enhancements showed a
rapid decrease with height, while the NO + OH reaction and aerosol-related
HONO sources decreased slowly with height. Photnitrate contributions to
HONO concentrations were enhanced with aggravated pollution levels. The enhancement of
HONO due to Photnitrate on hazy days was about 10 times greater than on
clean days and Photnitrate dominated daytime HONO sources
(∼ 30 %–70 % when the ratio of the photolysis frequency of
nitrate (Jnitrate) to gas nitric acid (JHNO3) equals 30) at higher
layers (>800 m). Compared with that on clean days, the
Photnitrate contribution to the enhanced daily maximum 8 h averaged
(DMA8) O3 was increased by over 1 magnitude during the haze-aggravating process. Photnitrate contributed only ∼ 5 %
of the surface HONO in the daytime with a Jnitrate/JHNO3 ratio of 30
but contributed ∼ 30 %–50 % of the enhanced O3 near the
surface in NCP on hazy days. Surface O3 was dominated by volatile
organic compound-sensitive chemistry, while O3 at higher altitudes
(>800 m) was dominated by NOx-sensitive chemistry.
Photnitrate had a limited impact on nitrate concentrations (<15 %) even with a Jnitrate/JHNO3 ratio of 120. These results
suggest the potential but significant impact of Photnitrate on O3
formation, and that more comprehensive studies on Photnitrate in the
atmosphere are still needed.