Unraveling the daytime source of molecular chlorine in the extra-polar
atmosphere
Abstract
Chlorine atoms (Cl) are highly reactive and can strongly influence
atmospheric abundances of climate and air quality-relevant trace gases
such as methane and ozone (O3). Despite extensive research on molecular
chlorine (Cl2), an important Cl atom precursor, in the polar atmosphere,
its sources in other regions are still poorly understood. Here we report
unprecedented levels of daytime Cl2 (up to 1 ppbv, the highest
atmospheric concentration ever reported, with an average of
~400 pptv) in a coastal area in Hong Kong, indicating
the presence of a large daytime source (Cl2 ~2.7 pptv/s
at noon) as the lifetime of Cl2 is only ~7 minutes at
noon. Field and laboratory results reveal that photolysis of particulate
nitrate under acidic conditions (pH <3.0) can activate
chloride and account for the observed daytime Cl2 production. The high
Cl2 concentrations observed at the site increased the atmospheric
oxidation rate of volatile organic compounds (VOCs) by 24 to 132%, ROx
radical by 4-27%, and daytime O3 integrated production by 17%. Given
the ubiquitous existence of chloride, nitrate, and acidic aerosols, we
propose that nitrate photolysis is a significant daytime chlorine source
globally. This so far unaccounted for a new source of chlorine can have
substantial impacts on global atmospheric chemistry.