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Mardi AH, Dadashazar H, MacDonald AB, Crosbie E, Coggon MM, Aghdam MA, Woods RK, Jonsson HH, Flagan RC, Seinfeld JH, Sorooshian A. Effects of Biomass Burning on Stratocumulus Droplet Characteristics, Drizzle Rate, and Composition. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2019; 124:12301-12318. [PMID: 33274175 PMCID: PMC7709909 DOI: 10.1029/2019jd031159] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/12/2019] [Accepted: 10/29/2019] [Indexed: 05/30/2023]
Abstract
This study reports on airborne measurements of stratocumulus cloud properties under varying degrees of influence from biomass burning (BB) plumes off the California coast. Data are reported from five total airborne campaigns based in Marina, California, with two of them including influence from wildfires in different areas along the coast of the western United States. The results indicate that subcloud cloud condensation nuclei number concentration and mass concentrations of important aerosol species (organics, sulfate, nitrate) were better correlated with cloud droplet number concentration (N d) as compared to respective above-cloud aerosol data. Given that the majority of BB particles resided above cloud tops, this is an important consideration for future work in the region as the data indicate that the subcloud BB particles likely were entrained from the free troposphere. Lower cloud condensation nuclei activation fractions were observed for BB-impacted clouds as compared to non-BB clouds due, at least partly, to less hygroscopic aerosols. Relationships between N d and either droplet effective radius or drizzle rate are preserved regardless of BB influence, indicative of how parameterizations can exhibit consistent skill for varying degrees of BB influence as long as N d is known. Lastly, the composition of both droplet residual particles and cloud water changed significantly when clouds were impacted by BB plumes, with differences observed for different fire sources stemming largely from effects of plume aging time and dust influence.
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Affiliation(s)
- 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
| | - Alexander B MacDonald
- 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
| | - Matthew M Coggon
- Cooperative Institute for Research in Environmental Science and National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Mojtaba Azadi Aghdam
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, USA
| | - Roy K Woods
- Naval Postgraduate School, Monterey, CA, 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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Korhonen H, Carslaw KS, Spracklen DV, Ridley DA, Ström J. A global model study of processes controlling aerosol size distributions in the Arctic spring and summer. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2007jd009114] [Citation(s) in RCA: 63] [Impact Index Per Article: 3.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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O'Dowd CD, Jimenez JL, Bahreini R, Flagan RC, Seinfeld JH, Hämeri K, Pirjola L, Kulmala M, Jennings SG, Hoffmann T. Marine aerosol formation from biogenic iodine emissions. Nature 2002; 417:632-6. [PMID: 12050661 DOI: 10.1038/nature00775] [Citation(s) in RCA: 281] [Impact Index Per Article: 12.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Abstract
The formation of marine aerosols and cloud condensation nuclei--from which marine clouds originate--depends ultimately on the availability of new, nanometre-scale particles in the marine boundary layer. Because marine aerosols and clouds scatter incoming radiation and contribute a cooling effect to the Earth's radiation budget, new particle production is important in climate regulation. It has been suggested that sulphuric acid derived from the oxidation of dimethyl sulphide is responsible for the production of marine aerosols and cloud condensation nuclei. It was accordingly proposed that algae producing dimethyl sulphide play a role in climate regulation, but this has been difficult to prove and, consequently, the processes controlling marine particle formation remains largely undetermined. Here, using smog chamber experiments under coastal atmospheric conditions, we demonstrate that new particles can form from condensable iodine-containing vapours, which are the photolysis products of biogenic iodocarbons emitted from marine algae. Moreover, we illustrate, using aerosol formation models, that concentrations of condensable iodine-containing vapours over the open ocean are sufficient to influence marine particle formation. We suggest therefore that marine iodocarbon emissions have a potentially significant effect on global radiative forcing.
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Affiliation(s)
- Colin D O'Dowd
- Department of Physics, National University of Ireland, Galway,
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Chapter 18 Formation and cycling of aerosols in the global troposphere. ACTA ACUST UNITED AC 2002. [DOI: 10.1016/s1474-8177(02)80021-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register]
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Weber RJ, Chen G, Davis DD, Mauldin RL, Tanner DJ, Eisele FL, Clarke AD, Thornton DC, Bandy AR. Measurements of enhanced H2SO4and 3-4 nm particles near a frontal cloud during the First Aerosol Characterization Experiment (ACE 1). ACTA ACUST UNITED AC 2001. [DOI: 10.1029/2000jd000109] [Citation(s) in RCA: 79] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Song CH, Carmichael GR. A three-dimensional modeling investigation of the evolution processes of dust and sea-salt particles in east Asia. ACTA ACUST UNITED AC 2001. [DOI: 10.1029/2000jd900352] [Citation(s) in RCA: 124] [Impact Index Per Article: 5.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Pirjola L, O'Dowd CD, Brooks IM, Kulmala M. Can new particle formation occur in the clean marine boundary layer? ACTA ACUST UNITED AC 2000. [DOI: 10.1029/2000jd900310] [Citation(s) in RCA: 84] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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