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Schulze BC, Charan SM, Kenseth CM, Kong W, Bates KH, Williams W, Metcalf AR, Jonsson HH, Woods R, Sorooshian A, Flagan RC, Seinfeld JH. Characterization of Aerosol Hygroscopicity Over the Northeast Pacific Ocean: Impacts on Prediction of CCN and Stratocumulus Cloud Droplet Number Concentrations. EARTH AND SPACE SCIENCE (HOBOKEN, N.J.) 2020; 7:e2020EA001098. [PMID: 33225018 PMCID: PMC7676499 DOI: 10.1029/2020ea001098] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 02/10/2020] [Accepted: 05/23/2020] [Indexed: 06/11/2023]
Abstract
During the Marine Aerosol Cloud and Wildfire Study (MACAWS) in June and July of 2018, aerosol composition and cloud condensation nuclei (CCN) properties were measured over the N.E. Pacific to characterize the influence of aerosol hygroscopicity on predictions of ambient CCN and stratocumulus cloud droplet number concentrations (CDNC). Three vertical regions were characterized, corresponding to the marine boundary layer (MBL), an above-cloud organic aerosol layer (AC-OAL), and the free troposphere (FT) above the AC-OAL. The aerosol hygroscopicity parameter (κ) was calculated from CCN measurements (κ CCN) and bulk aerosol mass spectrometer (AMS) measurements (κ AMS). Within the MBL, measured hygroscopicities varied between values typical of both continental environments (~0.2) and remote marine locations (~0.7). For most flights, CCN closure was achieved within 20% in the MBL. For five of the seven flights, assuming a constant aerosol size distribution produced similar or better CCN closure than assuming a constant "marine" hygroscopicity (κ = 0.72). An aerosol-cloud parcel model was used to characterize the sensitivity of predicted stratocumulus CDNC to aerosol hygroscopicity, size distribution properties, and updraft velocity. Average CDNC sensitivity to accumulation mode aerosol hygroscopicity is 39% as large as the sensitivity to the geometric median diameter in this environment. Simulations suggest CDNC sensitivity to hygroscopicity is largest in marine stratocumulus with low updraft velocities (<0.2 m s-1), where accumulation mode particles are most relevant to CDNC, and in marine stratocumulus or cumulus with large updraft velocities (>0.6 m s-1), where hygroscopic properties of the Aitken mode dominate hygroscopicity sensitivity.
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Affiliation(s)
- B. C. Schulze
- Department of Environmental Science and Engineering, California Institute of Technology, Pasadena, CA, USA
| | - S. M. Charan
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - C. M. Kenseth
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - W. Kong
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - K. H. Bates
- Center for the Environment, Harvard University, Cambridge, MA, USA
| | - W. Williams
- Department of Environmental Engineering and Earth Sciences, Clemson University, Anderson, SC, USA
| | - A. R. Metcalf
- Department of Environmental Engineering and Earth Sciences, Clemson University, Anderson, SC, USA
| | | | - R. Woods
- Naval Postgraduate School, Monterey, CA, USA
| | - A. Sorooshian
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, USA
| | - R. C. Flagan
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
- Division of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USA
| | - J. H. Seinfeld
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
- Division of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USA
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MacDonald AB, Hossein Mardi A, Dadashazar H, Azadi Aghdam M, Crosbie E, Jonsson HH, Flagan RC, Seinfeld JH, Sorooshian A. On the relationship between cloud water composition and cloud droplet number concentration. ATMOSPHERIC CHEMISTRY AND PHYSICS 2020; 20:7645-7665. [PMID: 33273899 PMCID: PMC7709908 DOI: 10.5194/acp-20-7645-2020] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Aerosol-cloud interactions are the largest source of uncertainty in quantifying anthropogenic radiative forcing. The large uncertainty is, in part, due to the difficulty of predicting cloud microphysical parameters, such as the cloud droplet number concentration (N d). Even though rigorous first-principle approaches exist to calculate N d, the cloud and aerosol research community also relies on empirical approaches such as relating N d to aerosol mass concentration. Here we analyze relationships between N d and cloud water chemical composition, in addition to the effect of environmental factors on the degree of the relationships. Warm, marine, stratocumulus clouds off the California coast were sampled throughout four summer campaigns between 2011 and 2016. A total of 385 cloud water samples were collected and analyzed for 80 chemical species. Single- and multispecies log-log linear regressions were performed to predict N d using chemical composition. Single-species regressions reveal that the species that best predicts N d is total sulfate (R adj 2 = 0.40 ). Multispecies regressions reveal that adding more species does not necessarily produce a better model, as six or more species yield regressions that are statistically insignificant. A commonality among the multispecies regressions that produce the highest correlation with N d was that most included sulfate (either total or non-sea-salt), an ocean emissions tracer (such as sodium), and an organic tracer (such as oxalate). Binning the data according to turbulence, smoke influence, and in-cloud height allowed for examination of the effect of these environmental factors on the composition-N d correlation. Accounting for turbulence, quantified as the standard deviation of vertical wind speed, showed that the correlation between N d with both total sulfate and sodium increased at higher turbulence conditions, consistent with turbulence promoting the mixing between ocean surface and cloud base. Considering the influence of smoke significantly improved the correlation with N d for two biomass burning tracer species in the study region, specifically oxalate and iron. When binning by in-cloud height, non-sea-salt sulfate and sodium correlated best with N d at cloud top, whereas iron and oxalate correlated best with N d at cloud base.
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Affiliation(s)
- Alexander B. MacDonald
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
| | - Ali Hossein Mardi
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
| | - Hossein Dadashazar
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
| | - Mojtaba Azadi Aghdam
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
| | - Ewan Crosbie
- Science Systems and Applications, Inc., Hampton, VA, USA
- NASA Langley Research Center, Hampton, VA, USA
| | | | - Richard C. Flagan
- Department of Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - John H. Seinfeld
- Department of Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - Armin Sorooshian
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, USA
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Sorooshian A, Corral AF, Braun RA, Cairns B, Crosbie E, Ferrare R, Hair J, Kleb MM, Mardi AH, Maring H, McComiskey A, Moore R, Painemal D, Jo Scarino A, Schlosser J, Shingler T, Shook M, Wang H, Zeng X, Ziemba L, Zuidema P. Atmospheric Research Over the Western North Atlantic Ocean Region and North American East Coast: A Review of Past Work and Challenges Ahead. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2020; 125:10.1029/2019jd031626. [PMID: 32699733 PMCID: PMC7375207 DOI: 10.1029/2019jd031626] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/12/2019] [Accepted: 01/21/2020] [Indexed: 05/26/2023]
Abstract
Decades of atmospheric research have focused on the Western North Atlantic Ocean (WNAO) region because of its unique location that offers accessibility for airborne and ship measurements, gradients in important atmospheric parameters, and a range of meteorological regimes leading to diverse conditions that are poorly understood. This work reviews these scientific investigations for the WNAO region, including the East Coast of North America and the island of Bermuda. Over 50 field campaigns and long-term monitoring programs, in addition to 715 peer-reviewed publications between 1946 and 2019 have provided a firm foundation of knowledge for these areas. Of particular importance in this region has been extensive work at the island of Bermuda that is host to important time series records of oceanic and atmospheric variables. Our review categorizes WNAO atmospheric research into eight major categories, with some studies fitting into multiple categories (relative %): Aerosols (25%), Gases (24%), Development/Validation of Techniques, Models, and Retrievals (18%), Meteorology and Transport (9%), Air-Sea Interactions (8%), Clouds/Storms (8%), Atmospheric Deposition (7%), and Aerosol-Cloud Interactions (2%). Recommendations for future research are provided in the categories highlighted above.
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Affiliation(s)
- Armin Sorooshian
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ
| | - Andrea F. Corral
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | - Rachel A. Braun
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | - Brian Cairns
- NASA Goddard Institute for Space Studies, New York, NY
| | - Ewan Crosbie
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | | | | | | | - Ali Hossein Mardi
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | | | | | | | - David Painemal
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | - Amy Jo Scarino
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | - Joseph Schlosser
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | | | | | - Hailong Wang
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA
| | - Xubin Zeng
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ
| | | | - Paquita Zuidema
- Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL
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4
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Influence of Common Assumptions Regarding Aerosol Composition and Mixing State on Predicted CCN Concentration. ATMOSPHERE 2018. [DOI: 10.3390/atmos9020054] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
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5
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Elemental Mixing State of Aerosol Particles Collected in Central Amazonia during GoAmazon2014/15. ATMOSPHERE 2017. [DOI: 10.3390/atmos8090173] [Citation(s) in RCA: 25] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
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6
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Schill S, Collins DB, Lee C, Morris HS, Novak GA, Prather KA, Quinn P, Sultana CM, Tivanski AV, Zimmermann K, Cappa CD, Bertram TH. The Impact of Aerosol Particle Mixing State on the Hygroscopicity of Sea Spray Aerosol. ACS CENTRAL SCIENCE 2015; 1:132-41. [PMID: 27162963 PMCID: PMC4827553 DOI: 10.1021/acscentsci.5b00174] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/25/2015] [Indexed: 05/03/2023]
Abstract
Aerosol particles influence global climate by determining cloud droplet number concentrations, brightness, and lifetime. Primary aerosol particles, such as those produced from breaking waves in the ocean, display large particle-particle variability in chemical composition, morphology, and physical phase state, all of which affect the ability of individual particles to accommodate water and grow into cloud droplets. Despite such diversity in molecular composition, there is a paucity of methods available to assess how particle-particle variability in chemistry translates to corresponding differences in aerosol hygroscopicity. Here, an approach has been developed that allows for characterization of the distribution of aerosol hygroscopicity within a chemically complex population of atmospheric particles. This methodology, when applied to the interpretation of nascent sea spray aerosol, provides a quantitative framework for connecting results obtained using molecular mimics generated in the laboratory with chemically complex ambient aerosol. We show that nascent sea spray aerosol, generated in situ in the Atlantic Ocean, displays a broad distribution of particle hygroscopicities, indicative of a correspondingly broad distribution of particle chemical compositions. Molecular mimics of sea spray aerosol organic material were used in the laboratory to assess the volume fractions and molecular functionality required to suppress sea spray aerosol hygroscopicity to the extent indicated by field observations. We show that proper accounting for the distribution and diversity in particle hygroscopicity and composition are important to the assessment of particle impacts on clouds and global climate.
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Affiliation(s)
- Steven
R. Schill
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
| | - Douglas B. Collins
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
| | - Christopher Lee
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
| | - Holly S. Morris
- Department
of Chemistry, University of Iowa, Iowa City, Iowa 52242, United States
| | - Gordon A. Novak
- Department
of Chemistry, University of Wisconsin Madison, Madison, Wisconsin 53706, United States
| | - Kimberly A. Prather
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
- Scripps
Institution of Oceanography, La
Jolla, California 92037, United States
| | - Patricia
K. Quinn
- Pacific
Marine Environmental Laboratory, National
Oceanic and Atmospheric Administration, Seattle, Washington 98115, United States
| | - Camille M. Sultana
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
| | - Alexei V. Tivanski
- Department
of Chemistry, University of Iowa, Iowa City, Iowa 52242, United States
| | - Kathryn Zimmermann
- Department
of Chemistry and Biochemistry, University
of California San Diego, La Jolla, California 92093, United States
| | - Christopher D. Cappa
- Department
of Civil and Environmental Engineering, University of California Davis, Davis, California 95616, United States
| | - Timothy H. Bertram
- Department
of Chemistry, University of Wisconsin Madison, Madison, Wisconsin 53706, United States
- E-mail:
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Zelenyuk A, Imre D, Wilson J, Zhang Z, Wang J, Mueller K. Airborne single particle mass spectrometers (SPLAT II & miniSPLAT) and new software for data visualization and analysis in a geo-spatial context. JOURNAL OF THE AMERICAN SOCIETY FOR MASS SPECTROMETRY 2015; 26:257-270. [PMID: 25563475 DOI: 10.1007/s13361-014-1043-4] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/06/2014] [Revised: 10/27/2014] [Accepted: 10/31/2014] [Indexed: 06/04/2023]
Abstract
Understanding the effect of aerosols on climate requires knowledge of the size and chemical composition of individual aerosol particles-two fundamental properties that determine an aerosol's optical properties and ability to serve as cloud condensation or ice nuclei. Here we present our aircraft-compatible single particle mass spectrometers, SPLAT II and its new, miniaturized version, miniSPLAT that measure in-situ and in real-time the size and chemical composition of individual aerosol particles with extremely high sensitivity, temporal resolution, and sizing precision on the order of a monolayer. Although miniSPLAT's size, weight, and power consumption are significantly smaller, its performance is on par with SPLAT II. Both instruments operate in dual data acquisition mode to measure, in addition to single particle size and composition, particle number concentrations, size distributions, density, and asphericity with high temporal resolution. We also present ND-Scope, our newly developed interactive visual analytics software package. ND-Scope is designed to explore and visualize the vast amount of complex, multidimensional data acquired by our single particle mass spectrometers, along with other aerosol and cloud characterization instruments on-board aircraft. We demonstrate that ND-Scope makes it possible to visualize the relationships between different observables and to view the data in a geo-spatial context, using the interactive and fully coupled Google Earth and Parallel Coordinates displays. Here we illustrate the utility of ND-Scope to visualize the spatial distribution of atmospheric particles of different compositions, and explore the relationship between individual particle compositions and their activity as cloud condensation nuclei.
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Affiliation(s)
- Alla Zelenyuk
- Pacific Northwest National Laboratory, Richland, WA, 99354, USA,
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8
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Ching J, Riemer N, West M. Impacts of black carbon mixing state on black carbon nucleation scavenging: Insights from a particle-resolved model. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd018269] [Citation(s) in RCA: 30] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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9
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Kristensen TB, Wex H, Nekat B, Nøjgaard JK, van Pinxteren D, Lowenthal DH, Mazzoleni LR, Dieckmann K, Bender Koch C, Mentel TF, Herrmann H, Gannet Hallar A, Stratmann F, Bilde M. Hygroscopic growth and CCN activity of HULIS from different environments. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd018249] [Citation(s) in RCA: 28] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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10
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Pratt KA, Prather KA. Mass spectrometry of atmospheric aerosols--recent developments and applications. Part II: On-line mass spectrometry techniques. MASS SPECTROMETRY REVIEWS 2012; 31:17-48. [PMID: 21449003 DOI: 10.1002/mas.20330] [Citation(s) in RCA: 48] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/09/2009] [Revised: 08/19/2010] [Accepted: 08/19/2010] [Indexed: 05/30/2023]
Abstract
Many of the significant advances in our understanding of atmospheric particles can be attributed to the application of mass spectrometry. Mass spectrometry provides high sensitivity with fast response time to probe chemically complex particles. This review focuses on recent developments and applications in the field of mass spectrometry of atmospheric aerosols. In Part II of this two-part review, we concentrate on real-time mass spectrometry techniques, which provide high time resolution for insight into brief events and diurnal changes while eliminating the potential artifacts acquired during long-term filter sampling. In particular, real-time mass spectrometry has been shown recently to provide the ability to probe the chemical composition of ambient individual particles <30 nm in diameter to further our understanding of how particles are formed through nucleation in the atmosphere. Further, transportable real-time mass spectrometry techniques are now used frequently on ground-, ship-, and aircraft-based studies around the globe to further our understanding of the spatial distribution of atmospheric aerosols. In addition, coupling aerosol mass spectrometry techniques with other measurements in series has allowed the in situ determination of chemically resolved particle effective density, refractive index, volatility, and cloud activation properties.
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Affiliation(s)
- Kerri A Pratt
- Department of Chemistry and Biochemistry, University of California, San Diego, La Jolla, California 92093, USA
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11
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Asa-Awuku A, Moore RH, Nenes A, Bahreini R, Holloway JS, Brock CA, Middlebrook AM, Ryerson TB, Jimenez JL, DeCarlo PF, Hecobian A, Weber RJ, Stickel R, Tanner DJ, Huey LG. Airborne cloud condensation nuclei measurements during the 2006 Texas Air Quality Study. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd014874] [Citation(s) in RCA: 75] [Impact Index Per Article: 5.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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12
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Jurányi Z, Gysel M, Weingartner E, Bukowiecki N, Kammermann L, Baltensperger U. A 17 month climatology of the cloud condensation nuclei number concentration at the high alpine site Jungfraujoch. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd015199] [Citation(s) in RCA: 59] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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13
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Barahona D, Sotiropoulou R, Nenes A. Global distribution of cloud droplet number concentration, autoconversion rate, and aerosol indirect effect under diabatic droplet activation. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd015274] [Citation(s) in RCA: 19] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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14
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Anttila T. Sensitivity of cloud droplet formation to the numerical treatment of the particle mixing state. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2010jd013995] [Citation(s) in RCA: 13] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Zaveri RA, Barnard JC, Easter RC, Riemer N, West M. Particle-resolved simulation of aerosol size, composition, mixing state, and the associated optical and cloud condensation nuclei activation properties in an evolving urban plume. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jd013616] [Citation(s) in RCA: 92] [Impact Index Per Article: 6.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/13/2023]
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16
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Stratmann F, Bilde M, Dusek U, Frank GP, Hennig T, Henning S, Kiendler-Scharr A, Kiselev A, Kristensson A, Lieberwirth I, Mentel TF, Pöschl U, Rose D, Schneider J, Snider JR, Tillmann R, Walter S, Wex H. Examination of laboratory-generated coated soot particles: An overview of the LACIS Experiment in November (LExNo) campaign. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jd012628] [Citation(s) in RCA: 23] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Lance S, Nenes A, Mazzoleni C, Dubey MK, Gates H, Varutbangkul V, Rissman TA, Murphy SM, Sorooshian A, Flagan RC, Seinfeld JH, Feingold G, Jonsson HH. Cloud condensation nuclei activity, closure, and droplet growth kinetics of Houston aerosol during the Gulf of Mexico Atmospheric Composition and Climate Study (GoMACCS). ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2008jd011699] [Citation(s) in RCA: 75] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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18
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Murphy SM, Agrawal H, Sorooshian A, Padró LT, Gates H, Hersey S, Welch WA, Lung H, Miller JW, Cocker DR, Nenes A, Jonsson HH, Flagan RC, Seinfeld JH. Comprehensive simultaneous shipboard and airborne characterization of exhaust from a modern container ship at sea. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2009; 43:4626-4640. [PMID: 19673244 DOI: 10.1021/es802413j] [Citation(s) in RCA: 28] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
We report the first joint shipboard and airborne study focused on the chemical composition and water-uptake behavior of particulate ship emissions. The study focuses on emissions from the main propulsion engine of a Post-Panamax class container ship cruising off the central coast of California and burning heavy fuel oil. Shipboard sampling included micro-orifice uniform deposit impactors (MOUDI) with subsequent off-line analysis, whereas airborne measurements involved a number of real-time analyzers to characterize the plume aerosol, aged from a few seconds to over an hour. The mass ratio of particulate organic carbon to sulfate at the base of the ship stack was 0.23 +/- 0.03, and increased to 0.30 +/- 0.01 in the airborne exhaust plume, with the additional organic mass in the airborne plume being concentrated largely in particles below 100 nm in diameter. The organic to sulfate mass ratio in the exhaust aerosol remained constant during the first hour of plume dilution into the marine boundary layer. The mass spectrum of the organic fraction of the exhaust aerosol strongly resembles that of emissions from other diesel sources and appears to be predominantly hydrocarbon-like organic (HOA) material. Background aerosol which, based on air mass back trajectories, probably consisted of aged ship emissions and marine aerosol, contained a lower organic mass fraction than the fresh plume and had a much more oxidized organic component. A volume-weighted mixing rule is able to accurately predict hygroscopic growth factors in the background aerosol but measured and calculated growth factors do not agree for aerosols in the ship exhaust plume. Calculated CCN concentrations, at supersaturations ranging from 0.1 to 0.33%, agree well with measurements in the ship-exhaust plume. Using size-resolved chemical composition instead of bulk submicrometer composition has little effect on the predicted CCN concentrations because the cutoff diameter for CCN activation is larger than the diameter where the mass fraction of organic aerosol begins to increase significantly. The particle number emission factor estimated from this study is 1.3 x 10(16) (kg fuel)(-1), with less than 1/10 of the particles having diameters above 100 nm; 24% of particles (>10 nm in diameter) activate into cloud droplets at 0.3% supersaturation.
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Affiliation(s)
- Shane M Murphy
- Department of Environmental Science and Engineering, California Institute of Technology, Pasadena, California 91125, USA
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Prather KA, Hatch CD, Grassian VH. Analysis of atmospheric aerosols. ANNUAL REVIEW OF ANALYTICAL CHEMISTRY (PALO ALTO, CALIF.) 2008; 1:485-514. [PMID: 20636087 DOI: 10.1146/annurev.anchem.1.031207.113030] [Citation(s) in RCA: 58] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/29/2023]
Abstract
Aerosols represent an important component of the Earth's atmosphere. Because aerosols are composed of solid and liquid particles of varying chemical complexity, size, and phase, large challenges exist in understanding how they impact climate, health, and the chemistry of the atmosphere. Only through the integration of field, laboratory, and modeling analysis can we begin to unravel the roles atmospheric aerosols play in these global processes. In this article, we provide a brief review of the current state of the science in the analysis of atmospheric aerosols and some important challenges that need to be overcome before they can become fully integrated. It is clear that only when these areas are effectively bridged can we fully understand the impact that atmospheric aerosols have on our environment and the Earth's system at the level of scientific certainty necessary to design and implement sound environmental policies.
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Affiliation(s)
- Kimberly A Prather
- Department of Chemistry and Biochemistry, Scripps Institution of Oceanography, University of California, San Diego, 92093-0314, USA.
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20
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Asa-Awuku A, Nenes A. Effect of solute dissolution kinetics on cloud droplet formation: Extended Köhler theory. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2005jd006934] [Citation(s) in RCA: 47] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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21
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Sotiropoulou REP, Nenes A, Adams PJ, Seinfeld JH. Cloud condensation nuclei prediction error from application of Köhler theory: Importance for the aerosol indirect effect. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd007834] [Citation(s) in RCA: 38] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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22
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Fountoukis C, Nenes A, Meskhidze N, Bahreini R, Conant WC, Jonsson H, Murphy S, Sorooshian A, Varutbangkul V, Brechtel F, Flagan RC, Seinfeld JH. Aerosol-cloud drop concentration closure for clouds sampled during the International Consortium for Atmospheric Research on Transport and Transformation 2004 campaign. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd007272] [Citation(s) in RCA: 87] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Christos Fountoukis
- School of Chemical and Biomolecular Engineering; Georgia Institute of Technology; Atlanta Georgia USA
| | - Athanasios Nenes
- School of Chemical and Biomolecular Engineering; Georgia Institute of Technology; Atlanta Georgia USA
| | - Nicholas Meskhidze
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - Roya Bahreini
- Environmental Science and Engineering; California Institute of Technology; Pasadena California USA
| | - William C. Conant
- Environmental Science and Engineering; California Institute of Technology; Pasadena California USA
| | - Haflidi Jonsson
- Center for Interdisciplinary Remotely-Piloted Aircraft Studies; Naval Postgraduate School; Monterey California USA
| | - Shane Murphy
- Department of Chemical Engineering; California Institute of Technology; Pasadena California USA
| | - Armin Sorooshian
- Department of Chemical Engineering; California Institute of Technology; Pasadena California USA
| | - Varuntida Varutbangkul
- Department of Chemical Engineering; California Institute of Technology; Pasadena California USA
| | - Fred Brechtel
- Environmental Science and Engineering; California Institute of Technology; Pasadena California USA
| | - Richard C. Flagan
- Environmental Science and Engineering; California Institute of Technology; Pasadena California USA
| | - John H. Seinfeld
- Environmental Science and Engineering; California Institute of Technology; Pasadena California USA
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23
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Fehsenfeld FC, Ancellet G, Bates TS, Goldstein AH, Hardesty RM, Honrath R, Law KS, Lewis AC, Leaitch R, McKeen S, Meagher J, Parrish DD, Pszenny AAP, Russell PB, Schlager H, Seinfeld J, Talbot R, Zbinden R. International Consortium for Atmospheric Research on Transport and Transformation (ICARTT): North America to Europe-Overview of the 2004 summer field study. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2006jd007829] [Citation(s) in RCA: 205] [Impact Index Per Article: 11.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
| | - G. Ancellet
- Service d'Aéronomie du Centre Nationale de la Recherche Scientifique; Institut Pierre Simon Laplace/Université Pierre et Marie Curie; Paris France
| | - T. S. Bates
- Pacific Marine Environmental Laboratory; NOAA; Seattle Washington USA
| | - A. H. Goldstein
- Department of Environmental Science, Policy and Management; University of California; Berkeley California USA
| | - R. M. Hardesty
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - R. Honrath
- Department of Civil and Environmental Engineering; Michigan Technological University; Houghton Michigan USA
| | - K. S. Law
- Service d'Aéronomie du Centre Nationale de la Recherche Scientifique; Institut Pierre Simon Laplace/Université Pierre et Marie Curie; Paris France
| | - A. C. Lewis
- Department of Chemistry; University of York; York UK
| | - R. Leaitch
- Science and Technology Branch; Environment Canada; Toronto, Ontario Canada
| | - S. McKeen
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - J. Meagher
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - D. D. Parrish
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - A. A. P. Pszenny
- Institute for the Study of Earth, Oceans and Space; University of New Hampshire; Durham New Hampshire USA
| | - P. B. Russell
- NASA Ames Research Center; Moffett Field California USA
| | - H. Schlager
- Deutsches Zentrum für Luft- und Raumfahrt; Oberpfaffenhofen, Wessling Germany
| | - J. Seinfeld
- Departments of Environmental Science and Engineering and Chemical Engineering; California Institute of Technology; Pasadena California USA
| | - R. Talbot
- Institute for the Study of Earth, Oceans and Space; University of New Hampshire; Durham New Hampshire USA
| | - R. Zbinden
- Laboratoire d'Aérologie, Observatoire Midi-Pyrénées; UMR 5560, Centre Nationale de la Recherche Scientifique/Université Paul Sabatier; Toulouse France
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