The significant contribution of HONO to secondary pollutants during a severe winter pollution event in southern China
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Published:2019-01-02
Issue:1
Volume:19
Page:1-14
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Fu XiaoORCID, Wang TaoORCID, Zhang LiORCID, Li QinyiORCID, Wang ZheORCID, Xia MenORCID, Yun Hui, Wang WeihaoORCID, Yu Chuan, Yue Dingli, Zhou Yan, Zheng Junyun, Han RuiORCID
Abstract
Abstract. Nitrous acid (HONO) can strongly affect atmospheric
photochemistry in polluted regions through the production of hydroxyl
radicals (OHs). In January 2017, a severe pollution episode occurred in the Pearl River
Delta (PRD) of China, with maximum hourly PM2.5, ozone, and HONO levels
reaching 400 µg m−3, 150 ppb, and 8 ppb, respectively, at a
suburban site. The present study investigated the sources
and processes
generating such high HONO concentrations and the role of HONO chemistry in
this severe winter episode. Four recently reported HONO sources were added to
the Community Multiscale Air Quality (CMAQ) model, including RH-dependent
(relative humidity) and light-enhancing effects on heterogeneous reactions, photolysis of
particulate nitrate in the atmosphere, and photolysis of HNO3 and
nitrate on surfaces. The revised model reproduced the observed HONO and
significantly improved its performance for O3 and PM2.5. The
model simulations showed that the heterogeneous generation on surfaces (with
RH and light effects) was the largest contributor (72 %) to the predicted
HONO concentrations, with the RH-enhancing effects more significant at
nighttime and the light-enhancing effects more important in the daytime. The
photolysis of total nitrate in the atmosphere and deposited on surfaces was
the dominant HONO source during noon and afternoon, contributing above 50 %
of the simulated HONO. The HONO photolysis was the dominant contributor to
HOx production in this episode. With all HONO sources, the
daytime average O3 at the Heshan site was increased by 24 ppb (or
70 %), compared to the simulation results without any HONO sources.
Moreover, the simulated mean concentrations of TNO3 (HNO3+
fine particle NO3-) at the Heshan site, which was the key species
for this haze formation, increased by about 17 µg m−3
(67 %) due to the HONO chemistry, and the peak enhancement reached
55 µg m−3. This study highlights the key role of HONO
chemistry in the formation of winter haze in a subtropical environment.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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