TY - JOUR
T1 - Fogs and air quality on the Southern California coast
AU - Boris, Alexandra J.
AU - Napolitano, Denise C.
AU - Herckes, Pierre
AU - Clements, Andrea L.
AU - Collett, Jeffrey L.
N1 - Funding Information:
This work was made possible through funding provided by a National Science Foundation (NSF). Purchase of the ESI-HR-ToF-MS system was supported through an NSF MRI grant (ATM-0521643). The authors gratefully acknowledge the following contributors to this study: Yong Zhou at Colorado State University Atmospheric Science Department for analysis of trace gases in whole-air grab samples, Amber Weir of Serra Cross Park for access to and use of the Serra Cross site for aerosol sampling, Daniel Lindsey of the National Oceanographic and Atmospheric Administration Center for Satellite Applications and Research for retrieval and processing of GOES-West satellite imagery, the laboratory of John (Nick) D. Fisk in the Chemistry Department of CSU for use of a Labteq fluorescence plate reader, and the NOAA Air Resources Laboratory (ARL) for the provision of the HySPLIT transport and dispersion model (http://www.ready.noaa.gov) used in this publication.
Publisher Copyright:
© Taiwan Association for Aerosol Research.
PY - 2018/1
Y1 - 2018/1
N2 - Fog acts as a reservoir and transport vector for chemicals in the atmosphere, altering the distribution of species between the gas and particle phases, and allowing deposition of nutrients and pollutants onto ecosystems and crops. Fog water and trace gas samples were collected from Casitas Pass along the Santa Barbara Channel in June 2015 to identify emissions sources and aqueous processes impacting Southern California air. Fog water composition was dominated by NH4+ (volume weighted mean, VWM = 232 µM, range = 85–640 µM), with lesser contributions from NO3– (126 µM, 30.4–778 µM) and SO42– (28.3 µM, 12.1–90.0 µM), pushing the VWM pH to 5.92 (5.34–6.67). Organic carbon contributed substantially to fog composition (8.27 mg C L–1, 4.70–16.8 mg C L–1). Carboxylic acids, products of aqueous oxidation, were abundant (20.1% of carbon mass on average), with > 1% contributions by acetate, formate, oxalate, malonate, succinate, and lactate. Sulfur- and nitrogen-containing organic species were detected, often after 3–5 hours of fog, suggesting aqueous formation. Sampled air was advected over the coastline near oil extraction operations, urban and agricultural areas; regional oil and natural gas processing and mobile sources were the most influential organic emissions at Casitas Pass. Fog composition in 2015 was contrasted with that from a study in July-September 1985/6. Concentrations of major fog constituents appear to have decreased in response to successful air quality regulations. While natural species concentrations in fog were similar (e.g., 2015 VWM [Na+ ] = 101 µM, range = < 30–320 µM; 1985/6 [Na+] = 129 µM, 12–1000 µM), anthropogenic species concentrations were lower in 2015 (e.g., 1985/6: [NO3–] = 236 µM, 141–2800 µM vs. 2015: 126 µM, 30.4–778 µM). These results overall highlight changes in Southern California air quality issues, including improvement of some anthropogenic emissions and the current influence of organic emissions from industrial and mobile sources.
AB - Fog acts as a reservoir and transport vector for chemicals in the atmosphere, altering the distribution of species between the gas and particle phases, and allowing deposition of nutrients and pollutants onto ecosystems and crops. Fog water and trace gas samples were collected from Casitas Pass along the Santa Barbara Channel in June 2015 to identify emissions sources and aqueous processes impacting Southern California air. Fog water composition was dominated by NH4+ (volume weighted mean, VWM = 232 µM, range = 85–640 µM), with lesser contributions from NO3– (126 µM, 30.4–778 µM) and SO42– (28.3 µM, 12.1–90.0 µM), pushing the VWM pH to 5.92 (5.34–6.67). Organic carbon contributed substantially to fog composition (8.27 mg C L–1, 4.70–16.8 mg C L–1). Carboxylic acids, products of aqueous oxidation, were abundant (20.1% of carbon mass on average), with > 1% contributions by acetate, formate, oxalate, malonate, succinate, and lactate. Sulfur- and nitrogen-containing organic species were detected, often after 3–5 hours of fog, suggesting aqueous formation. Sampled air was advected over the coastline near oil extraction operations, urban and agricultural areas; regional oil and natural gas processing and mobile sources were the most influential organic emissions at Casitas Pass. Fog composition in 2015 was contrasted with that from a study in July-September 1985/6. Concentrations of major fog constituents appear to have decreased in response to successful air quality regulations. While natural species concentrations in fog were similar (e.g., 2015 VWM [Na+ ] = 101 µM, range = < 30–320 µM; 1985/6 [Na+] = 129 µM, 12–1000 µM), anthropogenic species concentrations were lower in 2015 (e.g., 1985/6: [NO3–] = 236 µM, 141–2800 µM vs. 2015: 126 µM, 30.4–778 µM). These results overall highlight changes in Southern California air quality issues, including improvement of some anthropogenic emissions and the current influence of organic emissions from industrial and mobile sources.
KW - Aqueous atmospheric chemistry
KW - Aqueous secondary organic aerosol
KW - Fog chemistry
KW - Organic nitrogen
KW - Organic sulfur
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U2 - 10.4209/aaqr.2016.11.0522
DO - 10.4209/aaqr.2016.11.0522
M3 - Article
AN - SCOPUS:85040970058
SN - 1680-8584
VL - 18
SP - 224
EP - 239
JO - Aerosol and Air Quality Research
JF - Aerosol and Air Quality Research
IS - 1
ER -