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Lee JY, Peterson PK, Vear LR, Cook RD, Sullivan AP, Smith E, Hawkins LN, Olson NE, Hems R, Snyder PK, Pratt KA. Wildfire Smoke Influence on Cloud Water Chemical Composition at Whiteface Mountain, New York. J Geophys Res Atmos 2022; 127:e2022JD037177. [PMID: 36590830 PMCID: PMC9787799 DOI: 10.1029/2022jd037177] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 05/23/2022] [Revised: 09/16/2022] [Accepted: 09/26/2022] [Indexed: 06/17/2023]
Abstract
Wildfires significantly impact air quality and climate, including through the production of aerosols that can nucleate cloud droplets and participate in aqueous-phase reactions. Cloud water was collected during the summer months (June-September) of 2010-2017 at Whiteface Mountain, New York and examined for biomass burning influence. Cloud water samples were classified by their smoke influence based on backward air mass trajectories and satellite-detected smoke. A total of 1,338 cloud water samples collected over 485 days were classified by their probability of smoke influence, with 49% of these days categorized as having moderate to high probability of smoke influence. Carbon monoxide and ozone levels were enhanced during smoke influenced days at the summit of Whiteface Mountain. Smoke-influenced cloud water samples were characterized by enhanced concentrations of potassium, sulfate, ammonium, and total organic carbon, compared to samples lacking identified influence. Five cloud water samples were examined further for the presence of dissolved organic compounds, insoluble particles, and light-absorbing components. The five selected cloud water samples contained the biomass burning tracer levoglucosan at 0.02-0.09 μM. Samples influenced by air masses that remained aloft, above the boundary layer during transport, had lower insoluble particle concentrations, larger insoluble particle diameters, and larger oxalate:sulfate ratios, suggesting cloud processing had occurred. These findings highlight the influence that local and long-range transported smoke have on cloud water composition.
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Affiliation(s)
- Jamy Y. Lee
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
| | - Peter K. Peterson
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
- Now at Department of ChemistryWhittier CollegeWhittierCAUSA
| | - Logan R. Vear
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
| | - Ryan D. Cook
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
| | - Amy P. Sullivan
- Department of Atmospheric ScienceColorado State UniversityFort CollinsCOUSA
| | - Ellie Smith
- Department of ChemistryHarvey Mudd CollegeClaremontCAUSA
| | | | | | - Rachel Hems
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
| | | | - Kerri A. Pratt
- Department of ChemistryUniversity of MichiganAnn ArborMIUSA
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
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Koffman BG, Saylor P, Zhong R, Sethares L, Yoder MF, Hanschka L, Methven T, Cai Y, Bolge L, Longman J, Goldstein SL, Osterberg EC. Provenance of Anthropogenic Pb and Atmospheric Dust to Northwestern North America. Environ Sci Technol 2022; 56:13107-13118. [PMID: 36083611 PMCID: PMC9494742 DOI: 10.1021/acs.est.2c03767] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 05/25/2022] [Revised: 08/29/2022] [Accepted: 08/29/2022] [Indexed: 06/15/2023]
Abstract
Industrial activities release aerosols containing toxic metals into the atmosphere, where they are transported far from their sources, impacting ecosystems and human health. Concomitantly, long-range-transported mineral dust aerosols play a role in Earth's radiative balance and supply micronutrients to iron-limited ecosystems. To evaluate the sources of dust and pollutant aerosols to Alaska following the 2001 phase-out of leaded gasoline in China, we measured Pb-Sr-Nd isotopic compositions of particles collected in 2016 from snow pits across an elevational transect (2180-5240 m-a.s.l) in Denali National Park, USA. We also determined Pb flux and enrichment from 1991-2011 in the Denali ice core (3870 m-a.s.l). Chinese coal-burning and non-ferrous metal smelting account for up to 64% of Pb deposition at our sites, a value consistent across the western Arctic. Pb isotope ratios in the aerosols did not change between 2001 and 2016, despite the ban on lead additives. Emissions estimates demonstrate that industrial activities have more than compensated for the phase-out of leaded gasoline, with China emitting ∼37,000 metric tons year-1 of Pb during 2013-2015, approximately 78% of the Pb from East Asia. The Pb flux to Alaska now equals that measured in southern Greenland during peak pollution from North America.
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Affiliation(s)
- Bess G. Koffman
- Department
of Geology, Colby College, Waterville, Maine 04901, United States
| | - Patrick Saylor
- National
Center for Atmospheric Research, Boulder, Colorado 80307, United States
- Earth
Science Department, Dartmouth College, Hanover, New Hampshire 03755, United States
| | - Roujia Zhong
- Department
of Computer Science, Colby College, Waterville, Maine 04901, United States
| | - Lily Sethares
- Department
of Geology, Colby College, Waterville, Maine 04901, United States
| | - Meg F. Yoder
- Department
of Geology, Colby College, Waterville, Maine 04901, United States
- Department
of Earth and Environmental Sciences, Boston
College, Boston, Massachusetts 02467, United States
| | - Lena Hanschka
- Department
of Geology, Colby College, Waterville, Maine 04901, United States
| | - Taylor Methven
- Department
of Geology, Colby College, Waterville, Maine 04901, United States
| | - Yue Cai
- State
Key
Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Chinese Academy of
Sciences, Nanjing, Jiangsu Province 210008, P.R. China
- Lamont-Doherty
Earth Observatory of Columbia University, Palisades, New York 10964, United States
| | - Louise Bolge
- Lamont-Doherty
Earth Observatory of Columbia University, Palisades, New York 10964, United States
| | - Jack Longman
- Institute
for Chemistry and Biology of the Marine Environment, University of Oldenburg, 26129 Oldenburg, Germany
| | - Steven L. Goldstein
- Lamont-Doherty
Earth Observatory of Columbia University, Palisades, New York 10964, United States
- Department
of Earth and Environmental Sciences, Columbia
University, New York, New York 10027, United
States
| | - Erich C. Osterberg
- Earth
Science Department, Dartmouth College, Hanover, New Hampshire 03755, United States
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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 Space Sci 2020; 7:e2020EA001098. [PMID: 33225018 PMCID: PMC7676499 DOI: 10.1029/2020ea001098] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [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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Mahish M, Jefferson A, Collins D. Influence of Common Assumptions Regarding Aerosol Composition and Mixing State on Predicted CCN Concentration. Atmosphere 2018; 9:54. [DOI: 10.3390/atmos9020054] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
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Son SC, Park SS. Evaluating the applicability of a semi-continuous aerosol sampler to measure Asian dust particles. Environ Sci Process Impacts 2015; 17:561-569. [PMID: 25601751 DOI: 10.1039/c4em00404c] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/04/2023]
Abstract
A Korean prototype semi-continuous aerosol sampler was used to measure Asian dust particles. During two dust-storm periods, concentrations of crustal and trace elements were significantly enriched. Dust storms are one of the most significant natural sources of air pollution in East Asia. The present study aimed to evaluate use of a Korean semi-continuous aerosol sampler (K-SAS) in observation of mineral dust particles during dust storm events. Aerosol slurry samples were collected at 60 min intervals using the K-SAS, which was operated at a sampling flow rate of 16.7 L min(-1) through a PM10 cyclone inlet. The measurements were made during dust storm events at an urban site, Gwangju in Korea, between April 30 and May 5, 2011. The K-SAS uses particle growth technology as a means of collecting atmospheric aerosol particles. Concentrations of 16 elements (Al, Fe, Mn, Ca, K, Cu, Zn, Pb, Cd, Cr, Ti, V, Ni, Co, As, and Se) were determined off-line in the collected slurry samples by inductively coupled plasma-mass spectrometry (ICP-MS). The sampling periods were classified into two types, based on the source regions of the dust storms and the transport pathways of the air masses reaching the sampling site. The first period "A" was associated with dust particles with high Ca content, originating from the Gobi desert regions of northern China and southern Mongolia. The second period "B" was associated with dust particles with low Ca content, originating from northeastern Chinese sandy deserts. The results from the K-SAS indicated noticeable differences in concentrations of crustal and trace elements in the two sampling periods, as a result of differences in the source regions of the dust storms, the air mass transport pathways, and the impact of smoke from forest fires. The concentrations of the crustal (Al, Ca, Ti, Mn, and Fe) and anthropogenic trace elements (Vi, Ni, Cu, Zn, As, Se, and Pb) were enriched significantly during the two dust storm periods. However, the crustal elements were enriched more during dust storm period "A", whereas concentrations of the trace elements were higher during period "B". Higher concentrations of K during dust storm period "B" could be ascribed to smoke from forest fires, in addition to soil dust emissions. This result is supported by a strong correlation between the crustal elements and the K concentrations, higher K/Al and K/Fe ratios in period "B" than those detected in the soil samples from the Gobi desert regions and Chinese sandy deserts, and the smoke from forest fires. The results of this study indicate that the K-SAS is a good candidate for revealing the dynamics in the concentrations of elemental species in Asian dust particles, as well as in urban and industrial aerosols, and for developing insight into their sources.
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Affiliation(s)
- Se-Chang Son
- Department of Environment and Energy Engineering, Chonnam National University, 77 Yongbong-Ro, Buk-ku, Gwangju 500-757, Korea.
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Yin Y, Chen Q, Jin L, Chen B, Zhu S, Zhang X. The effects of deep convection on the concentration and size distribution of aerosol particles within the upper troposphere: A case study. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd017827] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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Moore RH, Cerully K, Bahreini R, Brock CA, Middlebrook AM, Nenes A. Hygroscopicity and composition of California CCN during summer 2010. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2011jd017352] [Citation(s) in RCA: 56] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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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] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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Mochida M, Nishita-Hara C, Furutani H, Miyazaki Y, Jung J, Kawamura K, Uematsu M. Hygroscopicity and cloud condensation nucleus activity of marine aerosol particles over the western North Pacific. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd014759] [Citation(s) in RCA: 44] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Wang SH, Lin NH, OuYang CF, Wang JL, Campbell JR, Peng CM, Lee CT, Sheu GR, Tsay SC. Impact of Asian dust and continental pollutants on cloud chemistry observed in northern Taiwan during the experimental period of ABC/EAREX 2005. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jd013692] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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Roberts GC, Ramana MV, Corrigan C, Kim D, Ramanathan V. Simultaneous observations of aerosol-cloud-albedo interactions with three stacked unmanned aerial vehicles. Proc Natl Acad Sci U S A 2008; 105:7370-5. [PMID: 18499803 DOI: 10.1073/pnas.0710308105] [Citation(s) in RCA: 47] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
Aerosol impacts on climate change are still poorly understood, in part, because the few observations and methods for detecting their effects are not well established. For the first time, the enhancement in cloud albedo is directly measured on a cloud-by-cloud basis and linked to increasing aerosol concentrations by using multiple autonomous unmanned aerial vehicles to simultaneously observe the cloud microphysics, vertical aerosol distribution, and associated solar radiative fluxes. In the presence of long-range transport of dust and anthropogenic pollution, the trade cumuli have higher droplet concentrations and are on average brighter. Our observations suggest a higher sensitivity of radiative forcing by trade cumuli to increases in cloud droplet concentrations than previously reported owing to a constrained droplet radius such that increases in droplet concentrations also increase cloud liquid water content. This aerosol-cloud forcing efficiency is as much as -60 W m(-2) per 100% percent cloud fraction for a doubling of droplet concentrations and associated increase of liquid water content. Finally, we develop a strategy for detecting aerosol-cloud interactions based on a nondimensional scaling analysis that relates the contribution of single clouds to albedo measurements and illustrates the significance of characterizing cloud morphology in resolving radiometric measurements. This study demonstrates that aerosol-cloud-albedo interactions can be directly observed by simultaneous observations below, in, and above the clouds.
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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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Holecek JC, Spencer MT, Prather KA. Analysis of rainwater samples: Comparison of single particle residues with ambient particle chemistry from the northeast Pacific and Indian oceans. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd008269] [Citation(s) in RCA: 20] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Yum SS, Roberts G, Kim JH, Song K, Kim D. Submicron aerosol size distributions and cloud condensation nuclei concentrations measured at Gosan, Korea, during the Atmospheric Brown Clouds–East Asian Regional Experiment 2005. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd008212] [Citation(s) in RCA: 53] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Ramanathan V, Li F, Ramana MV, Praveen PS, Kim D, Corrigan CE, Nguyen H, Stone EA, Schauer JJ, Carmichael GR, Adhikary B, Yoon SC. Atmospheric brown clouds: Hemispherical and regional variations in long-range transport, absorption, and radiative forcing. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd008124] [Citation(s) in RCA: 342] [Impact Index Per Article: 20.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Hadley OL, Ramanathan V, Carmichael GR, Tang Y, Corrigan CE, Roberts GC, Mauger GS. Trans-Pacific transport of black carbon and fine aerosols (D< 2.5μm) into North America. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd007632] [Citation(s) in RCA: 56] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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