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Pollution‐enhanced reactive chlorine chemistry in the eastern tropical Atlantic boundary layer
Author(s) -
Lawler M. J.,
Finley B. D.,
Keene W. C.,
Pszenny A. A. P.,
Read K. A.,
von Glasow R.,
Saltzman E. S.
Publication year - 2009
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2008gl036666
Subject(s) - cape verde , ozone , atmospheric chemistry , environmental chemistry , oceanography , tropical marine climate , plume , environmental science , tropical atlantic , aerosol , cycling , dimethyl sulfide , pollution , mineral dust , air pollution , atmospheric sciences , chemistry , geology , meteorology , geography , sea surface temperature , ecology , sulfur , ethnology , archaeology , organic chemistry , biology , history
This study examines atmospheric reactive chlorine chemistry at the Cape Verde Atmospheric Observatory in the eastern tropical Atlantic. During May–June, 2007, Cl 2 levels ranged from below detection (∼2 ppt) to 30 ppt. Elevated Cl 2 was associated with high HNO 3 (40 to 120 ppt) in polluted continental outflow transported in the marine boundary layer (MBL) to the site. Lower Cl 2 was observed in recently subsided air masses with multiday free tropospheric oceanic trajectories and in air containing Saharan dust. Model simulations show that the observations of elevated Cl 2 in polluted marine air are consistent with initiation of Cl chemistry by OH + HCl and subsequent heterogeneous, autocatalytic Cl cycling involving marine aerosols. Model estimates suggest that Cl atom reactions significantly impact the fates of methane and dimethylsulfide at Cape Verde and are moderately important for ozone cycling.