Observation of upper tropospheric sulfur dioxide- and acetone-pollution : Potential implications for hydroxyl radical and aerosol formation

• Published in: Geophysical research letters Vol. 24; no. 1; pp. 57 - 60
• Main Authors: ARNOLD, F, SCHNEIDER, J, GOLLINGER, K, SCHLAGER, H, SCHULTE, P, HAGEN, D. E, WHITEFIELD, P. D, VAN VELTHOVEN, P
• Format: Journal Article
• Language: English
• Published: Washington, DC American Geophysical Union 1997
• Subjects: Applied sciences; Atmospheric pollution; Chemical composition and interactions. Ionic interactions and processes; Earth, ocean, space; Exact sciences and technology; External geophysics; Meteorology; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution; Pollution; Atlantic Ocean; North Atlantic; Northeast Atlantic; Carbon dioxide; Troposphere; Condensation nucleus; Sulfur dioxide; Air mass; Long range pollutant transport; Aircraft observation; Aerosols; Air pollution; Trajectory; Hydroxyl; Acetone; Hydrogen Oxides
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/96GL03693

Aircraft-based measurements of sulfur dioxide, acetone, carbon dioxide, and condensation nuclei (CN) were made over the north-eastern Atlantic at upper tropospheric altitudes, around 9000 m. On October 14, 1993, strong SO sub(2) sub(-) and acetone-pollution (both up to 3 ppbv) were observed, which were accompanied by a CO sub(2) -enhancement of up to 6 ppmv, and large CN-concentrations of up to about 1500 cm super(-) super(3) (for radii greater than or equal to 6 nm). CN, excess CO sub(2) , and to a lesser degree also acetone, were positively correlated with SO sub(2) . Air mass trajectory analyses indicate, that most of the air masses encountered by our aircraft originated from the polluted planetary boundary layer of the North-Eastern U.S. approximately 4-5 days prior to our measurements, and that polluted boundary layer air experienced fast vertical transport to the upper troposphere as well as horizontal transport across the Atlantic. From our data we conclude, that in the polluted air mass around 9000 m altitude HO sub(x) -formation, photochemical SO sub(2) -conversion to gaseous H sub(2) SO sub(4) , and eventually also CN-formation by homogeneous bimolecular (H sub(2) SO sub(4) sub(-) H sub(2) O) nucleation may have taken place with enhanced efficiency.