globalchange  > 影响、适应和脆弱性
DOI: 10.1002/jgrd.50785
论文题名:
Measurements of submicron aerosols in Houston, Texas during the 2009 SHARP field campaign
作者: Levy M.E.; Zhang R.; Khalizov A.F.; Zheng J.; Collins D.R.; Glen C.R.; Wang Y.; Yu X.-Y.; Luke W.; Jayne J.T.; Olaguer E.
刊名: Journal of Geophysical Research Atmospheres
ISSN: 21698996
出版年: 2013
卷: 118, 期:18
起始页码: 10518
结束页码: 10534
语种: 英语
英文关键词: aerosol ; black carbon ; density ; hygroscopicity
Scopus关键词: Density (specific gravity) ; Mixing ; Particle size analysis ; Scattering ; Solar radiation ; Aerosol size distributions ; Black carbon ; Fine particulate matter ; hygroscopicity ; New particle formation ; Oxidation of organics ; Scattering co-efficient ; Single scattering albedo ; Aerosols ; aerosol property ; hygroscopicity ; light scattering ; measurement method ; meteorology ; optimization ; particle size ; particulate matter ; size distribution ; Houston ; Texas ; United States
英文摘要: During the field campaign of the Study of Houston Atmospheric Radical Precursors/Surface-Induced Oxidation of Organics in the Troposphere (SHARP/SOOT) in Houston, Texas, a suite of aerosol instruments was deployed to directly measure a comprehensive set of aerosol properties, including the particle size distribution, effective density, hygroscopicity, and light extinction and scattering coefficients. Those aerosol properties are employed to quantify the mixing state and composition of ambient particles and to gain a better understanding of the formation and transformation of fine particulate matter in this region. During the measurement period, aerosols are often internally mixed, with one peak in the effective density distribution at 1.55 ± 0.07 g cm-3, consistent with a population composed largely of sulfates and organics. Episodically, a second mode below 1.0 g cm-3 is identified in the effective density distributions, reflecting the presence of freshly emitted black carbon (BC) particles. The measured effective density demonstrates a clear diurnal cycle associated with primary emissions from transportation and photochemical aging, with a minimum during the morning rush hour, increasing from 1.4 to 1.5 g cm-3 on average over 5 h, and remaining nearly constant throughout the afternoon. The average BC concentration derived from light-absorption measurements is 0.31 ± 0.22 μg m-3, and the average measured particle single scattering albedo is 0.94 ± 0.04. When elevated BC concentrations are observed, typically during the morning rush hours, single scattering albedo decreases, with a smallest measured value of about 0.7. Aerosol hygroscopicity measurements indicate that larger particles (e.g., 400 nm) are more hygroscopic than smaller particles (e.g., 100 nm). The measurements also reveal discernable meteorological impacts on the aerosol properties. After a frontal passage, the average particle effective density decreases, the average BC concentration increases, and the aerosol size distribution is dominated by new particle formation. Key Points Quantification of the mixing state and composition of ambient particlesBetter understanding of formation and transformation of aerosolsDemonstration of meteorological impacts on aerosol properties ©2013. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/63298
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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作者单位: Department of Atmospheric Sciences, Texas AandM University, College Station, TX 77843, United States; School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing, China; Sandia National Laboratories, Albuquerque, NM, United States; Pacific Northwest National Laboratory, Richland, WA, United States; NOAA/Air Resources Laboratory, Silver Spring, MD, United States; Center for Aerosol and Cloud Chemistry, Aerodyne Research, Inc., Billerica, MA, United States; Houston Advanced Research Center, Houston, TX, United States

Recommended Citation:
Levy M.E.,Zhang R.,Khalizov A.F.,et al. Measurements of submicron aerosols in Houston, Texas during the 2009 SHARP field campaign[J]. Journal of Geophysical Research Atmospheres,2013-01-01,118(18)
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