Open AccessAerosol chemical composition in Asian continental outflow during the TRACE‐P campaign: Comparison with PEM‐West B
Author(s) -
Dibb Jack E.,
Talbot Robert W.,
Scheuer Eric M.,
Seid Garry,
Avery Melody A.,
Singh Hanwant B.
Publication year - 2003
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2002jd003111
Subject(s) - aerosol , troposphere , outflow , sink (geography) , precipitation , chemical composition , tracer , environmental science , atmospheric sciences , scavenging , trace gas , geology , chemistry , meteorology , physics , oceanography , geography , biochemistry , cartography , organic chemistry , nuclear physics , antioxidant
Aerosol associated soluble ions and the radionuclide tracers 7 Be and 210 Pb were quantified in 414 filter samples collected in spring 2001 from the DC‐8 during the Transport and Chemical Evolution over the Pacific (TRACE‐P) campaign. Binning the data into near Asia (flights from Hong Kong and Japan) and remote Pacific (all other flights) revealed large enhancements of NO 3 − , SO 4 = , C 2 O 4 = , NH 4 + , K + , Mg 2+ , and Ca 2+ near Asia. The boundary layer and lower troposphere were most strongly influenced by continental outflow, and the largest enhancements were seen in Ca 2+ (a dust tracer) and NO 3 − (reflecting uptake of HNO 3 onto the dust). Comparing the TRACE P near Asia bin with earlier results from the same region during PEM‐West B (in 1994) shows at least twofold enhancements during TRACE P in most of the ions listed above. Calcium and NO 3 − were most enhanced in this comparison as well (more than sevenfold higher in the boundary layer and threefold higher in the lower troposphere). Independent estimation of Asian emissions of gaseous precursors of the aerosol‐associated ions suggest only small changes between the two missions, and precipitation fields do not suggest any significant difference in the efficiency of the primary sink, precipitation scavenging. It thus appears that with the possible exception of dust, the enhancements of aerosol‐associated species during TRACE P cannot be explained by stronger sources or weaker sinks. We argue that the enhancements largely reflect the fact that TRACE P focused on characterizing Asian outflow, and thus the DC‐8 was more frequently flown into regions that were influenced by well‐organized flow off the continent.