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Lahti H, Kulmala M, Lyyra N, Mietola V, Paakkari L. Problematic situations related to social media use and competencies to prevent them: results of a Delphi study. Sci Rep 2024; 14:5275. [PMID: 38438460 PMCID: PMC10912411 DOI: 10.1038/s41598-024-55578-5] [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] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/05/2023] [Accepted: 02/26/2024] [Indexed: 03/06/2024] Open
Abstract
A three-round Delphi method was used to study the problematic situations that adolescents may encounter when using the social media, and the competencies needed to address these situations. A panel of Finnish experts (N = 22) provided an open-ended list of problematic situations and competencies in 2020-2021. These were then evaluated and ranked according to their significance. The experts provided an information-rich list of both problematic situations and competencies. Finally, 16 problematic situations and 19 competencies were ranked in order of importance by the experts. The most important problematic situations were direct and indirect cyberbullying and sexual harassment. The most important competencies were the ability to act responsibly, knowing what kinds of activity are prohibited, and knowing whom to contact on exposure to cyberbullying or harassment. The findings can be used in developing policies, recommendations, and solutions aimed at counteracting the harmful effects of social media on wellbeing during adolescence.
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Affiliation(s)
- H Lahti
- Faculty of Sport and Health Sciences, University of Jyväskylä, P.O. Box 35 (L), 40014, Jyväskylä, Finland.
| | - M Kulmala
- Faculty of Sport and Health Sciences, University of Jyväskylä, P.O. Box 35 (L), 40014, Jyväskylä, Finland
| | - N Lyyra
- Faculty of Sport and Health Sciences, University of Jyväskylä, P.O. Box 35 (L), 40014, Jyväskylä, Finland
| | - V Mietola
- Faculty of Sport and Health Sciences, University of Jyväskylä, P.O. Box 35 (L), 40014, Jyväskylä, Finland
| | - L Paakkari
- Faculty of Sport and Health Sciences, University of Jyväskylä, P.O. Box 35 (L), 40014, Jyväskylä, Finland
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2
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Paakkari L, Lahti H, Kulmala M, Paakkari O, Lyyra N. Health literacy among adolescents: summary of some key findings from ten European countries. Eur J Public Health 2022. [DOI: 10.1093/eurpub/ckac129.321] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/13/2022] Open
Abstract
Abstract
Introduction
In research on disparities, the concept of health literacy (HL) as a set of competencies to promote and sustain health may help in understanding the disparities better and in addressing avoidable and unfair health disparities. The presentation will present some key findings on adolescents’ HL levels in ten European countries, and how HL mediates and moderates between various background factors and health outcomes.
Methods
Data consisted of cross-sectional data from Health Behaviour in School-aged Children (HBSC) study from year 2017/18 of ten European countries (Austria, Belgium (Fl), Czechia, England, Estonia, Finland, Germany, Macedonia, Poland, and Slovakia). Data (n = 14,590 - 22,291) of 13- and 15-year-old pupils were used. Indicators include background variables (e.g. age, gender), Health literacy, Health indicators (e.g. self-rated health (SRH) and problematic social media use (PSMU)). Analysis include (1) Mediator analysis (with Mplus): pearson correlation coefficients, path models (Mplus 7.3 and Maximum Likelihood estimator) and (2) random effects models and moderator analyses (with R-sofware).
Findings
HL is an independent factor explaining disparities in health (e.g. SRH), and a mediator as well as a moderator between health outcomes and background factors. Based on the national analyses HL had significant main effects in every country, but group level differences emerged only in some countries. For instance, in Finland and Belgium, among girls HL lowered the likelihood to problematic social media use, but not among boys.
Discussion
HL is of use in understanding and tackling health disparities among adolescents. Results confirm the need to adopt the principles of proportionate universalism when promoting HL among adolescents to avoid widening the disparities within population groups. Also, country-specific health literacy interventions are needed to secure equity in opportunities of different population groups to benefit from the HL interventions.
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Affiliation(s)
- L Paakkari
- Faculty of Sport and Health Sciences, University of Jyväskylä , Jyväskylä, Finland
| | - H Lahti
- Faculty of Sport and Health Sciences, University of Jyväskylä , Jyväskylä, Finland
| | - M Kulmala
- Faculty of Sport and Health Sciences, University of Jyväskylä , Jyväskylä, Finland
| | - O Paakkari
- Faculty of Sport and Health Sciences, University of Jyväskylä , Jyväskylä, Finland
| | - N Lyyra
- Faculty of Sport and Health Sciences, University of Jyväskylä , Jyväskylä, Finland
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3
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Hakala S, Vakkari V, Bianchi F, Dada L, Deng C, Dällenbach KR, Fu Y, Jiang J, Kangasluoma J, Kujansuu J, Liu Y, Petäjä T, Wang L, Yan C, Kulmala M, Paasonen P. Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing. Environ Sci Atmos 2022; 2:146-164. [PMID: 35419523 PMCID: PMC8929417 DOI: 10.1039/d1ea00089f] [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] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 10/29/2021] [Accepted: 12/29/2021] [Indexed: 06/14/2023]
Abstract
Atmospheric aerosols have significant effects on the climate and on human health. New particle formation (NPF) is globally an important source of aerosols but its relevance especially towards aerosol mass loadings in highly polluted regions is still controversial. In addition, uncertainties remain regarding the processes leading to severe pollution episodes, concerning e.g. the role of atmospheric transport. In this study, we utilize air mass history analysis in combination with different fields related to the intensity of anthropogenic emissions in order to calculate air mass exposure to anthropogenic emissions (AME) prior to their arrival at Beijing, China. The AME is used as a semi-quantitative metric for describing the effect of air mass history on the potential for aerosol formation. We show that NPF events occur in clean air masses, described by low AME. However, increasing AME seems to be required for substantial growth of nucleation mode (diameter < 30 nm) particles, originating either from NPF or direct emissions, into larger mass-relevant sizes. This finding assists in establishing and understanding the connection between small nucleation mode particles, secondary aerosol formation and the development of pollution episodes. We further use the AME, in combination with basic meteorological variables, for developing a simple and easy-to-apply regression model to predict aerosol volume and mass concentrations. Since the model directly only accounts for changes in meteorological conditions, it can also be used to estimate the influence of emission changes on pollution levels. We apply the developed model to briefly investigate the effects of the COVID-19 lockdown on PM2.5 concentrations in Beijing. While no clear influence directly attributable to the lockdown measures is found, the results are in line with other studies utilizing more widely applied approaches.
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Affiliation(s)
- S Hakala
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
| | - V Vakkari
- Finnish Meteorological Institute Erik Palmenin Aukio 1 Helsinki Finland
- Atmospheric Chemistry Research Group, Chemical Resource Beneficiation, North-West University Potchefstroom South Africa
| | - F Bianchi
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
| | - L Dada
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
- Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL) Valais Sion 1951 Switzerland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - C Deng
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University Beijing China
| | - K R Dällenbach
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Y Fu
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University Beijing China
| | - J Jiang
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University Beijing China
| | - J Kangasluoma
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
| | - J Kujansuu
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
| | - Y Liu
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
| | - T Petäjä
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University Nanjing China
| | - L Wang
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences Beijing 100029 China
| | - C Yan
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
| | - M Kulmala
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University Nanjing China
| | - P Paasonen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland
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4
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Yan C, Nie W, Vogel AL, Dada L, Lehtipalo K, Stolzenburg D, Wagner R, Rissanen MP, Xiao M, Ahonen L, Fischer L, Rose C, Bianchi F, Gordon H, Simon M, Heinritzi M, Garmash O, Roldin P, Dias A, Ye P, Hofbauer V, Amorim A, Bauer PS, Bergen A, Bernhammer AK, Breitenlechner M, Brilke S, Buchholz A, Mazon SB, Canagaratna MR, Chen X, Ding A, Dommen J, Draper DC, Duplissy J, Frege C, Heyn C, Guida R, Hakala J, Heikkinen L, Hoyle CR, Jokinen T, Kangasluoma J, Kirkby J, Kontkanen J, Kürten A, Lawler MJ, Mai H, Mathot S, Mauldin RL, Molteni U, Nichman L, Nieminen T, Nowak J, Ojdanic A, Onnela A, Pajunoja A, Petäjä T, Piel F, Quéléver LLJ, Sarnela N, Schallhart S, Sengupta K, Sipilä M, Tomé A, Tröstl J, Väisänen O, Wagner AC, Ylisirniö A, Zha Q, Baltensperger U, Carslaw KS, Curtius J, Flagan RC, Hansel A, Riipinen I, Smith JN, Virtanen A, Winkler PM, Donahue NM, Kerminen VM, Kulmala M, Ehn M, Worsnop DR. Size-dependent influence of NO x on the growth rates of organic aerosol particles. Sci Adv 2020; 6:eaay4945. [PMID: 32518819 PMCID: PMC7253163 DOI: 10.1126/sciadv.aay4945] [Citation(s) in RCA: 22] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/01/2019] [Accepted: 03/19/2020] [Indexed: 05/24/2023]
Abstract
Atmospheric new-particle formation (NPF) affects climate by contributing to a large fraction of the cloud condensation nuclei (CCN). Highly oxygenated organic molecules (HOMs) drive the early particle growth and therefore substantially influence the survival of newly formed particles to CCN. Nitrogen oxide (NOx) is known to suppress the NPF driven by HOMs, but the underlying mechanism remains largely unclear. Here, we examine the response of particle growth to the changes of HOM formation caused by NOx. We show that NOx suppresses particle growth in general, but the suppression is rather nonuniform and size dependent, which can be quantitatively explained by the shifted HOM volatility after adding NOx. By illustrating how NOx affects the early growth of new particles, a critical step of CCN formation, our results help provide a refined assessment of the potential climatic effects caused by the diverse changes of NOx level in forest regions around the globe.
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Affiliation(s)
- C. Yan
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - W. Nie
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - A. L. Vogel
- CERN, CH-1211, Geneva, Switzerland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - L. Dada
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - K. Lehtipalo
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland
| | - D. Stolzenburg
- University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Wien, Austria
| | - R. Wagner
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - M. P. Rissanen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - M. Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - L. Ahonen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - L. Fischer
- University of Innsbruck, Institute for Ion and Applied Physics, 6020 Innsbruck, Austria
| | - C. Rose
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - F. Bianchi
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
| | - H. Gordon
- CERN, CH-1211, Geneva, Switzerland
- University of Leeds, Leeds LS2 9JT, UK
| | - M. Simon
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - M. Heinritzi
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - O. Garmash
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - P. Roldin
- Division of Nuclear Physics, Department of Physics, Lund University, P. O. Box 118, SE-221 00 Lund, Sweden
| | - A. Dias
- CERN, CH-1211, Geneva, Switzerland
- CENTRA and FCUL, Universidade de Lisboa, Campo Grande, 1749-016 Lisboa, Portugal
| | - P. Ye
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA 15213, USA
- Aerodyne Research Inc., Billerica, MA 01821, USA
| | - V. Hofbauer
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA 15213, USA
| | - A. Amorim
- CENTRA and FCUL, Universidade de Lisboa, Campo Grande, 1749-016 Lisboa, Portugal
| | - P. S. Bauer
- University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Wien, Austria
| | - A. Bergen
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - A.-K. Bernhammer
- University of Innsbruck, Institute for Ion and Applied Physics, 6020 Innsbruck, Austria
| | - M. Breitenlechner
- University of Innsbruck, Institute for Ion and Applied Physics, 6020 Innsbruck, Austria
| | - S. Brilke
- University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Wien, Austria
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - A. Buchholz
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
| | - S. Buenrostro Mazon
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | | | - X. Chen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - A. Ding
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - J. Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - D. C. Draper
- Department of Chemistry, University of California, Irvine, CA 92697, USA
| | - J. Duplissy
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - C. Frege
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - C. Heyn
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - R. Guida
- CERN, CH-1211, Geneva, Switzerland
| | - J. Hakala
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - L. Heikkinen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - C. R. Hoyle
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - T. Jokinen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - J. Kangasluoma
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
| | - J. Kirkby
- CERN, CH-1211, Geneva, Switzerland
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - J. Kontkanen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - A. Kürten
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - M. J. Lawler
- Department of Chemistry, University of California, Irvine, CA 92697, USA
| | - H. Mai
- California Institute of Technology, 210-41, Pasadena, CA 91125, USA
| | | | - R. L. Mauldin
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA 15213, USA
- Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO 80309, USA
| | - U. Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - L. Nichman
- School of Earth and Environmental Science, University of Manchester, Manchester M13 9PL, UK
| | - T. Nieminen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - J. Nowak
- Aerodyne Research Inc., Billerica, MA 01821, USA
| | - A. Ojdanic
- University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Wien, Austria
| | | | - A. Pajunoja
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
| | - T. Petäjä
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - F. Piel
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - L. L. J. Quéléver
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - N. Sarnela
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - S. Schallhart
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | | | - M. Sipilä
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - A. Tomé
- IDL Universidade da Beira Interior, Covilhã, Portugal
| | - J. Tröstl
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - O. Väisänen
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
| | - A. C. Wagner
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - A. Ylisirniö
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
| | - Q. Zha
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - U. Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | | | - J. Curtius
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
| | - R. C. Flagan
- California Institute of Technology, 210-41, Pasadena, CA 91125, USA
| | - A. Hansel
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- University of Innsbruck, Institute for Ion and Applied Physics, 6020 Innsbruck, Austria
- IONICON GesmbH, Innsbruck, Austria
| | - I. Riipinen
- Department of Environmental Science and Analytical Chemistry (ACES) and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
| | - J. N. Smith
- Department of Chemistry, University of California, Irvine, CA 92697, USA
| | - A. Virtanen
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
| | - P. M. Winkler
- University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Wien, Austria
| | - N. M. Donahue
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA 15213, USA
| | - V.-M. Kerminen
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - M. Kulmala
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
- Helsinki Institute of Physics, FI-00014 Helsinki, Finland
| | - M. Ehn
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
| | - D. R. Worsnop
- Institute for Atmospheric and Earth System Research/INAR–Physics, Faculty of Science, University of Helsinki, 00560 Helsinki, Finland
- Aerodyne Research Inc., Billerica, MA 01821, USA
- University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
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5
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Jokinen T, Sipilä M, Kontkanen J, Vakkari V, Tisler P, Duplissy EM, Junninen H, Kangasluoma J, Manninen HE, Petäjä T, Kulmala M, Worsnop DR, Kirkby J, Virkkula A, Kerminen VM. Ion-induced sulfuric acid-ammonia nucleation drives particle formation in coastal Antarctica. Sci Adv 2018; 4:eaat9744. [PMID: 30498779 PMCID: PMC6261657 DOI: 10.1126/sciadv.aat9744] [Citation(s) in RCA: 16] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/11/2018] [Accepted: 10/26/2018] [Indexed: 05/16/2023]
Abstract
Formation of new aerosol particles from trace gases is a major source of cloud condensation nuclei (CCN) in the global atmosphere, with potentially large effects on cloud optical properties and Earth's radiative balance. Controlled laboratory experiments have resolved, in detail, the different nucleation pathways likely responsible for atmospheric new particle formation, yet very little is known from field studies about the molecular steps and compounds involved in different regions of the atmosphere. The scarcity of primary particle sources makes secondary aerosol formation particularly important in the Antarctic atmosphere. Here, we report on the observation of ion-induced nucleation of sulfuric acid and ammonia-a process experimentally investigated by the CERN CLOUD experiment-as a major source of secondary aerosol particles over coastal Antarctica. We further show that measured high sulfuric acid concentrations, exceeding 107 molecules cm-3, are sufficient to explain the observed new particle growth rates. Our findings show that ion-induced nucleation is the dominant particle formation mechanism, implying that galactic cosmic radiation plays a key role in new particle formation in the pristine Antarctic atmosphere.
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Affiliation(s)
- T. Jokinen
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
- Corresponding author.
| | - M. Sipilä
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - J. Kontkanen
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - V. Vakkari
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland
| | - P. Tisler
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland
| | - E.-M. Duplissy
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - H. Junninen
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
- Laboratory of Environmental Physics, Institute of Physics, University of Tartu, Tartu 50090, Estonia
| | - J. Kangasluoma
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - H. E. Manninen
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
- CERN, CH1211 Geneva, Switzerland
| | - T. Petäjä
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - M. Kulmala
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
| | - D. R. Worsnop
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
- Aerodyne Research Inc., Billerica, MA 01821, USA
| | - J. Kirkby
- CERN, CH1211 Geneva, Switzerland
- Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, 60438 Frankfurt am Main, Germany
| | - A. Virkkula
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland
| | - V.-M. Kerminen
- INAR–Institute for Atmospheric and Earth System Research, P.O. Box 64, 00014 University of Helsinki, Finland
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6
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Dall'Osto M, Beddows DCS, Asmi A, Poulain L, Hao L, Freney E, Allan JD, Canagaratna M, Crippa M, Bianchi F, de Leeuw G, Eriksson A, Swietlicki E, Hansson HC, Henzing JS, Granier C, Zemankova K, Laj P, Onasch T, Prevot A, Putaud JP, Sellegri K, Vidal M, Virtanen A, Simo R, Worsnop D, O'Dowd C, Kulmala M, Harrison RM. Novel insights on new particle formation derived from a pan-european observing system. Sci Rep 2018; 8:1482. [PMID: 29367716 PMCID: PMC5784154 DOI: 10.1038/s41598-017-17343-9] [Citation(s) in RCA: 34] [Impact Index Per Article: 5.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/04/2017] [Accepted: 11/20/2017] [Indexed: 11/10/2022] Open
Abstract
The formation of new atmospheric particles involves an initial step forming stable clusters less than a nanometre in size (<~1 nm), followed by growth into quasi-stable aerosol particles a few nanometres (~1–10 nm) and larger (>~10 nm). Although at times, the same species can be responsible for both processes, it is thought that more generally each step comprises differing chemical contributors. Here, we present a novel analysis of measurements from a unique multi-station ground-based observing system which reveals new insights into continental-scale patterns associated with new particle formation. Statistical cluster analysis of this unique 2-year multi-station dataset comprising size distribution and chemical composition reveals that across Europe, there are different major seasonal trends depending on geographical location, concomitant with diversity in nucleating species while it seems that the growth phase is dominated by organic aerosol formation. The diversity and seasonality of these events requires an advanced observing system to elucidate the key processes and species driving particle formation, along with detecting continental scale changes in aerosol formation into the future.
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Affiliation(s)
- M Dall'Osto
- Institute of Marine Science, Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain. .,National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom. .,School of Physics, Centre for Climate & Air Pollution Studies, National University of Ireland Galway, University Road Galway, Galway, Ireland. .,Aerodyne Research, Inc., Billerica, MA, USA.
| | - D C S Beddows
- National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom
| | - A Asmi
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - L Poulain
- Leibniz Institute for Tropospheric Research, Permoserstr. 15, 04318, Leipzig, Germany
| | - L Hao
- University of Eastern Finland, Department of Applied Physics, P.O.Box 1627, FIN-70211, Kuopio, Finland
| | - E Freney
- Laboratoire de Météorologie Physique, CNRS-Université Blaise Pascal, UMR6016, 63117, Clermont, Ferrand, France
| | - J D Allan
- School of Earth, Atmospheric and Environmental Sciences, The University of Manchester, Manchester, UK
| | | | - M Crippa
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland.,European Commission, Joint Research Centre (JRC), Directorate for Energy, Transport and Climate, Air and Climate Unit, Via E. Fermi 2749, I-21027, Ispra, (VA), Italy
| | - F Bianchi
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.,Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland
| | - G de Leeuw
- Finnish Meteorological Institute, Climate Change Unit, P.O. Box 503, 00101, Helsinki, Finland.,Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands
| | - A Eriksson
- Division of Ergonomics and Aerosol Technology, Lund University, Box 118, SE-22100, Lund, Sweden
| | - E Swietlicki
- Division of Nuclear Physics, Lund University, Box 118, SE-22100, Lund, Sweden
| | - H C Hansson
- Department of Environmental Science and Analytical Chemistry, Stockholm University, 10691, Stockholm, Sweden
| | - J S Henzing
- Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands
| | - C Granier
- Laboratoire d'Aérologie, Toulouse, France.,NOAA Earth System Laboratory and CIRES, University of Colorado, Boulder, USA
| | - K Zemankova
- Charles University, Faculty of Mathematics and Physics, Dept. of Atmospheric Physcis, Prague, Czechia
| | - P Laj
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.,Univ. Grenoble-Alpes, CNRS, IRD, INPG, Institut des Géosciences de l'Environnement, Grenoble, France.,Univ. Grenoble-Alpes, CNRS, IRD, Observatoire des Sciences de l'Univers, Grenoble, France
| | - T Onasch
- Aerodyne Research, Inc., Billerica, MA, USA
| | - A Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland
| | - J P Putaud
- European Commission, Joint Research Centre, Institute for Environment and Sustainability, 21027, (VA), Italy
| | - K Sellegri
- Laboratoire de Météorologie Physique, CNRS-Université Blaise Pascal, UMR6016, 63117, Clermont, Ferrand, France
| | - M Vidal
- Department of Evolutionary Biology, Ecology and Environmental Sciences, Universitat de Barcelona, Av. Diagonal 643, 08028, Barcelona, Catalonia, Spain
| | - A Virtanen
- University of Eastern Finland, Department of Applied Physics, P.O.Box 1627, FIN-70211, Kuopio, Finland
| | - R Simo
- Institute of Marine Science, Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain
| | - D Worsnop
- Aerodyne Research, Inc., Billerica, MA, USA.,Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - C O'Dowd
- School of Physics, Centre for Climate & Air Pollution Studies, National University of Ireland Galway, University Road Galway, Galway, Ireland
| | - M Kulmala
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - Roy M Harrison
- National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom.,Department of Environmental Sciences / Center of Excellence in Environmental Studies, King Abdulaziz University, PO Box 80203, 21589, Jeddah, Saudi Arabia
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7
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Steiner G, Franchin A, Kangasluoma J, Kerminen VM, Kulmala M, Petäjä T. Production of neutral molecular clusters by controlled neutralization of mobility standards. Aerosol Sci Technol 2017; 51:946-955. [PMID: 28824221 PMCID: PMC5546065 DOI: 10.1080/02786826.2017.1328103] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/16/2016] [Revised: 02/09/2017] [Accepted: 04/04/2017] [Indexed: 06/07/2023]
Abstract
Measuring aerosols and molecular clusters below the 3 nm size limit is essential to increase our understanding of new particle formation. Instruments for the detection of sub-3 nm aerosols and clusters exist and need to be carefully calibrated and characterized. So far calibrations and laboratory tests have been carried out using mainly electrically charged aerosols, as they are easier to handle experimentally. However, the charging state of the cluster is an important variable to take into account. Furthermore, instrument characterization performed with charged aerosols could be biased, preventing a correct interpretation of data when electrically neutral sub-3 nm aerosols are involved. This article presents the first steps to generate electrically neutral molecular clusters as standards for calibration. We show two methods: One based on the neutralization of well-known molecular clusters (mobility standards) by ions generated in a switchable aerosol neutralizer. The second is based on the controlled neutralization of mobility standards with mobility standards of opposite polarity in a recombination cell. We highlight the challenges of these two techniques and, where possible, point out solutions. In addition, we give an outlook on the next steps toward generating well-defined neutral molecular clusters with a known chemical composition and concentration. Published with license by American Association for Aerosol Research.
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Affiliation(s)
- G. Steiner
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Faculty of Physics, University of Vienna, Wien, Austria
| | - A. Franchin
- Department of Physics, University of Helsinki, Helsinki, Finland
- Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado, USA
- National Oceanic and Atmospheric Administration (NOAA), Earth System Research Laboratory, Chemical Sciences Division, Boulder, Colorado, USA
| | - J. Kangasluoma
- Department of Physics, University of Helsinki, Helsinki, Finland
| | - V.-M. Kerminen
- Department of Physics, University of Helsinki, Helsinki, Finland
| | - M. Kulmala
- Department of Physics, University of Helsinki, Helsinki, Finland
| | - T. Petäjä
- Department of Physics, University of Helsinki, Helsinki, Finland
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8
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Kulmala M, Kerminen VM, Petäjä T, Ding AJ, Wang L. Atmospheric gas-to-particle conversion: why NPF events are observed in megacities? Faraday Discuss 2017; 200:271-288. [DOI: 10.1039/c6fd00257a] [Citation(s) in RCA: 91] [Impact Index Per Article: 13.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
In terms of the global aerosol particle number load, atmospheric new particle formation (NPF) dominates over primary emissions. The key for quantifying the importance of atmospheric NPF is to understand how gas-to-particle conversion (GTP) takes place at sizes below a few nanometers in particle diameter in different environments, and how this nano-GTP affects the survival of small clusters into larger sizes. The survival probability of growing clusters is tied closely to the competition between their growth and scavenging by pre-existing aerosol particles, and the key parameter in this respect is the ratio between the condensation sink (CS) and the cluster growth rate (GR). Here we define their ratio as a dimensionless survival parameter,P, asP= (CS/10−4s−1)/(GR/nm h−1). Theoretical arguments and observations in clean and moderately-polluted conditions indicate thatPneeds to be smaller than about 50 for a notable NPF to take place. However, the existing literature shows that in China, NPF occurs frequently in megacities such as in Beijing, Nanjing and Shanghai, and our analysis shows that the calculated values ofPare even larger than 200 in these cases. By combining direct observations and conceptual modelling, we explore the variability of the survival parameterPin different environments and probe the reasons for NPF occurrence under highly-polluted conditions.
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Affiliation(s)
- M. Kulmala
- University of Helsinki
- Department
- of Physics
- Finland
| | | | - T. Petäjä
- University of Helsinki
- Department
- of Physics
- Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences (JirLATEST)
| | - A. J. Ding
- Joint International Research Laboratory of Atmospheric and Earth System Sciences (JirLATEST)
- School of Atmospheric Sciences
- Nanjing University
- Nanjing
- China
| | - L. Wang
- Fudan University
- Department of Environmental Science and Engineering
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3)
- Shanghai 200433
- China
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9
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Dunne EM, Gordon H, Kurten A, Almeida J, Duplissy J, Williamson C, Ortega IK, Pringle KJ, Adamov A, Baltensperger U, Barmet P, Benduhn F, Bianchi F, Breitenlechner M, Clarke A, Curtius J, Dommen J, Donahue NM, Ehrhart S, Flagan RC, Franchin A, Guida R, Hakala J, Hansel A, Heinritzi M, Jokinen T, Kangasluoma J, Kirkby J, Kulmala M, Kupc A, Lawler MJ, Lehtipalo K, Makhmutov V, Mann G, Mathot S, Merikanto J, Miettinen P, Nenes A, Onnela A, Rap A, Reddington CLS, Riccobono F, Richards NAD, Rissanen MP, Rondo L, Sarnela N, Schobesberger S, Sengupta K, Simon M, Sipila M, Smith JN, Stozkhov Y, Tome A, Trostl J, Wagner PE, Wimmer D, Winkler PM, Worsnop DR, Carslaw KS. Global atmospheric particle formation from CERN CLOUD measurements. Science 2016; 354:1119-1124. [DOI: 10.1126/science.aaf2649] [Citation(s) in RCA: 213] [Impact Index Per Article: 26.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/18/2016] [Accepted: 10/12/2016] [Indexed: 11/03/2022]
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10
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Bianchi F, Tröstl J, Junninen H, Frege C, Henne S, Hoyle CR, Molteni U, Herrmann E, Adamov A, Bukowiecki N, Chen X, Duplissy J, Gysel M, Hutterli M, Kangasluoma J, Kontkanen J, Kürten A, Manninen HE, Münch S, Peräkylä O, Petäjä T, Rondo L, Williamson C, Weingartner E, Curtius J, Worsnop DR, Kulmala M, Dommen J, Baltensperger U. New particle formation in the free troposphere: A question of chemistry and timing. Science 2016; 352:1109-12. [PMID: 27226488 DOI: 10.1126/science.aad5456] [Citation(s) in RCA: 141] [Impact Index Per Article: 17.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/04/2015] [Accepted: 03/29/2016] [Indexed: 11/02/2022]
Abstract
New particle formation (NPF) is the source of over half of the atmosphere's cloud condensation nuclei, thus influencing cloud properties and Earth's energy balance. Unlike in the planetary boundary layer, few observations of NPF in the free troposphere exist. We provide observational evidence that at high altitudes, NPF occurs mainly through condensation of highly oxygenated molecules (HOMs), in addition to taking place through sulfuric acid-ammonia nucleation. Neutral nucleation is more than 10 times faster than ion-induced nucleation, and growth rates are size-dependent. NPF is restricted to a time window of 1 to 2 days after contact of the air masses with the planetary boundary layer; this is related to the time needed for oxidation of organic compounds to form HOMs. These findings require improved NPF parameterization in atmospheric models.
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Affiliation(s)
- F Bianchi
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland. Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland. Department of Physics, University of Helsinki, 00014 Helsinki, Finland.
| | - J Tröstl
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - H Junninen
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - C Frege
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - S Henne
- Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600 Dübendorf, Switzerland
| | - C R Hoyle
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland. WSL (Swiss Federal Institute for Forest, Snow and Landscape Research) Institute for Snow and Avalanche Research SLF, 7260 Davos, Switzerland
| | - U Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - E Herrmann
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - A Adamov
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - N Bukowiecki
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - X Chen
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - J Duplissy
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland. Helsinki Institute of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - M Gysel
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | | | - J Kangasluoma
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - J Kontkanen
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - A Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - H E Manninen
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - S Münch
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - O Peräkylä
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - T Petäjä
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - L Rondo
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - C Williamson
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - E Weingartner
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - J Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - D R Worsnop
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland. Aerodyne Research, Billerica, MA 01821, USA
| | - M Kulmala
- Department of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - J Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - U Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
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11
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Rondo L, Ehrhart S, Kürten A, Adamov A, Bianchi F, Breitenlechner M, Duplissy J, Franchin A, Dommen J, Donahue NM, Dunne EM, Flagan RC, Hakala J, Hansel A, Keskinen H, Kim J, Jokinen T, Lehtipalo K, Leiminger M, Praplan A, Riccobono F, Rissanen MP, Sarnela N, Schobesberger S, Simon M, Sipilä M, Smith JN, Tomé A, Tröstl J, Tsagkogeorgas G, Vaattovaara P, Winkler PM, Williamson C, Wimmer D, Baltensperger U, Kirkby J, Kulmala M, Petäjä T, Worsnop DR, Curtius J. Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass Spectrometry. J Geophys Res Atmos 2016; 121:3036-3049. [PMID: 27610289 PMCID: PMC4996328 DOI: 10.1002/2015jd023868] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/09/2015] [Revised: 10/15/2015] [Accepted: 11/09/2015] [Indexed: 06/06/2023]
Abstract
Sulfuric acid is widely recognized as a very important substance driving atmospheric aerosol nucleation. Based on quantum chemical calculations it has been suggested that the quantitative detection of gas phase sulfuric acid (H2SO4) by use of Chemical Ionization Mass Spectrometry (CIMS) could be biased in the presence of gas phase amines such as dimethylamine (DMA). An experiment (CLOUD7 campaign) was set up at the CLOUD (Cosmics Leaving OUtdoor Droplets) chamber to investigate the quantitative detection of H2SO4 in the presence of dimethylamine by CIMS at atmospherically relevant concentrations. For the first time in the CLOUD experiment, the monomer sulfuric acid concentration was measured by a CIMS and by two CI-APi-TOF (Chemical Ionization-Atmospheric Pressure interface-Time Of Flight) mass spectrometers. In addition, neutral sulfuric acid clusters were measured with the CI-APi-TOFs. The CLOUD7 measurements show that in the presence of dimethylamine (<5 to 70 pptv) the sulfuric acid monomer measured by the CIMS represents only a fraction of the total H2SO4, contained in the monomer and the clusters that is available for particle growth. Although it was found that the addition of dimethylamine dramatically changes the H2SO4 cluster distribution compared to binary (H2SO4-H2O) conditions, the CIMS detection efficiency does not seem to depend substantially on whether an individual H2SO4 monomer is clustered with a DMA molecule. The experimental observations are supported by numerical simulations based on A Self-contained Atmospheric chemistry coDe coupled with a molecular process model (Sulfuric Acid Water NUCleation) operated in the kinetic limit.
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12
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Elperin T, Kleeorin N, Krasovitov B, Kulmala M, Liberman M, Rogachevskii I, Zilitinkevich S. Acceleration of raindrop formation due to the tangling-clustering instability in a turbulent stratified atmosphere. Phys Rev E Stat Nonlin Soft Matter Phys 2015; 92:013012. [PMID: 26274274 DOI: 10.1103/physreve.92.013012] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/26/2015] [Indexed: 06/04/2023]
Abstract
Condensation of water vapor on active cloud condensation nuclei produces micron-size water droplets. To form rain, they must grow rapidly into at least 50- to 100-μm droplets. Observations show that this process takes only 15-20 min. The unexplained physical mechanism of such fast growth is crucial for understanding and modeling of rain and known as "condensation-coalescence bottleneck in rain formation." We show that the recently discovered phenomenon of the tangling clustering instability of small droplets in temperature-stratified turbulence [Phys. Fluids 25, 085104 (2013)] results in the formation of droplet clusters with drastically increased droplet number densities. The mechanism of the tangling clustering instability is much more effective than the previously considered by us the inertial clustering instability caused by the centrifugal effect of turbulent vortices. This is the reason of strong enhancement of the collision-coalescence rate inside the clusters. The mean-field theory of the droplet growth developed in this study can be useful for explanation of the observed fast growth of cloud droplets in warm clouds from the initial 1-μm-size droplets to 40- to 50-μm-size droplets within 15-20 min.
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Affiliation(s)
- T Elperin
- The Pearlstone Center for Aeronautical Engineering Studies, Department of Mechanical Engineering, Ben-Gurion University of the Negev, P. O. Box 653, Beer-Sheva 84105, Israel
| | - N Kleeorin
- The Pearlstone Center for Aeronautical Engineering Studies, Department of Mechanical Engineering, Ben-Gurion University of the Negev, P. O. Box 653, Beer-Sheva 84105, Israel
| | - B Krasovitov
- The Pearlstone Center for Aeronautical Engineering Studies, Department of Mechanical Engineering, Ben-Gurion University of the Negev, P. O. Box 653, Beer-Sheva 84105, Israel
| | - M Kulmala
- Division of Atmospheric Sciences, Department of Physics, P. O. Box 64, 00014 University of Helsinki, Finland
| | - M Liberman
- Nordita, KTH Royal Institute of Technology and Stockholm University, Roslagstullsbacken 23, 10691 Stockholm, Sweden
- Moscow Institute of Physics and Technology, Dolgoprudnyi, 141700, Russia
| | - I Rogachevskii
- The Pearlstone Center for Aeronautical Engineering Studies, Department of Mechanical Engineering, Ben-Gurion University of the Negev, P. O. Box 653, Beer-Sheva 84105, Israel
| | - S Zilitinkevich
- Division of Atmospheric Sciences, Department of Physics, P. O. Box 64, 00014 University of Helsinki, Finland
- Finnish Meteorological Institute (FMI) P. O. Box 503, 00101 Helsinki, Finland
- Department of Radio Physics, N. I. Lobachevsky State University of Nizhny Novgorod, Russia
- Moscow State University; Institute of Geography of Russian Academy of Sciences, Moscow, Russia
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13
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Lintunen A, Hölttä T, Kulmala M. Anatomical regulation of ice nucleation and cavitation helps trees to survive freezing and drought stress. Sci Rep 2014; 3:2031. [PMID: 23778457 PMCID: PMC3686780 DOI: 10.1038/srep02031] [Citation(s) in RCA: 27] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/28/2013] [Accepted: 05/31/2013] [Indexed: 11/25/2022] Open
Abstract
Water in the xylem, the water transport system of plants, is vulnerable to freezing and cavitation, i.e. to phase change from liquid to ice or gaseous phase. The former is a threat in cold and the latter in dry environmental conditions. Here we show that a small xylem conduit diameter, which has previously been shown to be associated with lower cavitation pressure thus making a plant more drought resistant, is also associated with a decrease in the temperature required for ice nucleation in the xylem. Thus the susceptibility of freezing and cavitation are linked together in the xylem of plants. We explain this linkage by the regulation of the sizes of the nuclei catalysing freezing and drought cavitation. Our results offer better understanding of the similarities of adaption of plants to cold and drought stress, and offer new insights into the ability of plants to adapt to the changing environment.
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Affiliation(s)
- A Lintunen
- Department of Forest Sciences, University of Helsinki, Helsinki, Finland.
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14
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Riccobono F, Schobesberger S, Scott CE, Dommen J, Ortega IK, Rondo L, Almeida J, Amorim A, Bianchi F, Breitenlechner M, David A, Downard A, Dunne EM, Duplissy J, Ehrhart S, Flagan RC, Franchin A, Hansel A, Junninen H, Kajos M, Keskinen H, Kupc A, Kurten A, Kvashin AN, Laaksonen A, Lehtipalo K, Makhmutov V, Mathot S, Nieminen T, Onnela A, Petaja T, Praplan AP, Santos FD, Schallhart S, Seinfeld JH, Sipila M, Spracklen DV, Stozhkov Y, Stratmann F, Tome A, Tsagkogeorgas G, Vaattovaara P, Viisanen Y, Vrtala A, Wagner PE, Weingartner E, Wex H, Wimmer D, Carslaw KS, Curtius J, Donahue NM, Kirkby J, Kulmala M, Worsnop DR, Baltensperger U. Oxidation Products of Biogenic Emissions Contribute to Nucleation of Atmospheric Particles. Science 2014; 344:717-21. [DOI: 10.1126/science.1243527] [Citation(s) in RCA: 397] [Impact Index Per Article: 39.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
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15
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Kulmala M, Petäjä T, Ehn M, Thornton J, Sipilä M, Worsnop D, Kerminen VM. Chemistry of Atmospheric Nucleation: On the Recent Advances on Precursor Characterization and Atmospheric Cluster Composition in Connection with Atmospheric New Particle Formation. Annu Rev Phys Chem 2014; 65:21-37. [DOI: 10.1146/annurev-physchem-040412-110014] [Citation(s) in RCA: 190] [Impact Index Per Article: 19.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- M. Kulmala
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
| | - T. Petäjä
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
| | - M. Ehn
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
- Institute for Energy and Climate Research (IEK-8), 52425 Jülich, Germany
| | - J. Thornton
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195
| | - M. Sipilä
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
| | - D.R. Worsnop
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
- Aerodyne Research, Inc., Billerica, Massachusetts 01821
| | - V.-M. Kerminen
- Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland;
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16
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Noppel M, Vehkamäki H, Winkler PM, Kulmala M, Wagner PE. Heterogeneous nucleation in multi-component vapor on a partially wettable charged conducting particle. II. The generalized Laplace, Gibbs-Kelvin, and Young equations and application to nucleation. J Chem Phys 2013; 139:134108. [DOI: 10.1063/1.4822047] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/15/2022] Open
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17
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Noppel M, Vehkamäki H, Winkler PM, Kulmala M, Wagner PE. Heterogeneous nucleation in multi-component vapor on a partially wettable charged conducting particle. I. Formulation of general equations: electrical surface and line excess quantities. J Chem Phys 2013; 139:134107. [PMID: 24116552 DOI: 10.1063/1.4822046] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
Abstract
Thermodynamics is applied to formulate general equations for internal energies and grand potential for a system consisting of a dielectric liquid nucleus of a new phase on a charged insoluble conducting sphere within a uniform macroscopic one- or multicomponent mother phase. The currently available model for ion-induced nucleation assumes complete spherical symmetry of the system, implying that the seed ion is immediately surrounded by the condensing liquid from all sides. We take a step further and treat more realistic geometries, where a cap-shaped liquid cluster forms on the surface of the seed particle. To take into account spontaneous polarization of surface layer molecules we introduce the electrical surface and line excess quantities.
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Affiliation(s)
- M Noppel
- Institute of Physics, University of Tartu, 18 Ülikooli St., 50090 Tartu, Estonia
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18
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Mauldin RL, Berndt T, Sipilä M, Paasonen P, Petäjä T, Kim S, Kurtén T, Stratmann F, Kerminen VM, Kulmala M. A new atmospherically relevant oxidant of sulphur dioxide. Nature 2012; 488:193-6. [PMID: 22874964 DOI: 10.1038/nature11278] [Citation(s) in RCA: 237] [Impact Index Per Article: 19.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/23/2011] [Accepted: 05/10/2012] [Indexed: 01/12/2023]
Abstract
Atmospheric oxidation is a key phenomenon that connects atmospheric chemistry with globally challenging environmental issues, such as climate change, stratospheric ozone loss, acidification of soils and water, and health effects of air quality. Ozone, the hydroxyl radical and the nitrate radical are generally considered to be the dominant oxidants that initiate the removal of trace gases, including pollutants, from the atmosphere. Here we present atmospheric observations from a boreal forest region in Finland, supported by laboratory experiments and theoretical considerations, that allow us to identify another compound, probably a stabilized Criegee intermediate (a carbonyl oxide with two free-radical sites) or its derivative, which has a significant capacity to oxidize sulphur dioxide and potentially other trace gases. This compound probably enhances the reactivity of the atmosphere, particularly with regard to the production of sulphuric acid, and consequently atmospheric aerosol formation. Our findings suggest that this new atmospherically relevant oxidation route is important relative to oxidation by the hydroxyl radical, at least at moderate concentrations of that radical. We also find that the oxidation chemistry of this compound seems to be tightly linked to the presence of alkenes of biogenic origin.
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Affiliation(s)
- R L Mauldin
- University of Helsinki, Department of Physics, FI-00014 Helsinki, Finland.
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19
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Bates TS, Quinn PK, Frossard AA, Russell LM, Hakala J, Petäjä T, Kulmala M, Covert DS, Cappa CD, Li SM, Hayden KL, Nuaaman I, McLaren R, Massoli P, Canagaratna MR, Onasch TB, Sueper D, Worsnop DR, Keene WC. Measurements of ocean derived aerosol off the coast of California. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd017588] [Citation(s) in RCA: 87] [Impact Index Per Article: 7.3] [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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20
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Baklanov A, Lawrence M, Pandis S, Mahura A, Finardi S, Moussiopoulos N, Beekmann M, Laj P, Gomes L, Jaffrezo JL, Borbon A, Coll I, Gros V, Sciare J, Kukkonen J, Galmarini S, Giorgi F, Grimmond S, Esau I, Stohl A, Denby B, Wagner T, Butler T, Baltensperger U, Builtjes P, van den Hout D, van der Gon HD, Collins B, Schluenzen H, Kulmala M, Zilitinkevich S, Sokhi R, Friedrich R, Theloke J, Kummer U, Jalkinen L, Halenka T, Wiedensholer A, Pyle J, Rossow WB. MEGAPOLI: concept of multi-scale modelling of megacity impact on air quality and climate. Adv Sci Res 2010. [DOI: 10.5194/asr-4-115-2010] [Citation(s) in RCA: 51] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/11/2022] Open
Abstract
Abstract. The EU FP7 Project MEGAPOLI: "Megacities: Emissions, urban, regional and Global Atmospheric POLlution and climate effects, and Integrated tools for assessment and mitigation" (http://megapoli.info) brings together leading European research groups, state-of-the-art scientific tools and key players from non-European countries to investigate the interactions among megacities, air quality and climate. MEGAPOLI bridges the spatial and temporal scales that connect local emissions, air quality and weather with global atmospheric chemistry and climate. The suggested concept of multi-scale integrated modelling of megacity impact on air quality and climate and vice versa is discussed in the paper. It requires considering different spatial and temporal dimensions: time scales from seconds and hours (to understand the interaction mechanisms) up to years and decades (to consider the climate effects); spatial resolutions: with model down- and up-scaling from street- to global-scale; and two-way interactions between meteorological and chemical processes.
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21
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Sinha V, Williams J, Lelieveld J, Ruuskanen TM, Kajos MK, Patokoski J, Hellen H, Hakola H, Mogensen D, Boy M, Rinne J, Kulmala M. OH reactivity measurements within a boreal forest: evidence for unknown reactive emissions. Environ Sci Technol 2010; 44:6614-6620. [PMID: 20687598 DOI: 10.1021/es101780b] [Citation(s) in RCA: 10] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/29/2023]
Abstract
Boreal forests emit large amounts of volatile organic compounds (VOCs) which react with the hydroxyl radical (OH) to influence regional ozone levels and form secondary organic aerosol. Using OH reactivity measurements within a boreal forest in Finland, we investigated the budget of reactive VOCs. OH reactivity was measured using the comparative reactivity method, whereas 30 individual VOCs were measured using proton transfer reaction mass spectrometry, thermal-desorption gas chromatography mass spectrometry, and liquid chromatography mass spectrometry, in August 2008. The measured OH reactivity ranged from below detection limit (3.5 s(-1)), to approximately 60 s(-1) in a single pollution event. The average OH reactivity was approximately 9 s(-1) and no diel variation was observed in the profiles. The measured OH sinks (approximately 30 species) accounted for only 50% of the total measured OH reactivity, implying unknown reactive VOCs within the forest. The five highest measured OH sinks were: monoterpenes (1 s(-1)), CO (0.7 s(-1)), isoprene (0.5 s(-1)), propanal and acetone (0.3 s(-1)), and methane (0.3 s(-1)). We suggest that models be constrained by direct OH reactivity measurements to accurately assess the impact of boreal forest emissions on regional atmospheric chemistry and climate.
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Affiliation(s)
- Vinayak Sinha
- Max Planck Institute for Chemistry, Department of Air Chemistry, P.O. Box 3060, 55020 Mainz, Germany.
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22
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Herrmann E, Brus D, Hyvärinen AP, Stratmann F, Wilck M, Lihavainen H, Kulmala M. A Computational Fluid Dynamics Approach to Nucleation in the Water−Sulfuric Acid System. J Phys Chem A 2010; 114:8033-42. [DOI: 10.1021/jp103499q] [Citation(s) in RCA: 20] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- E. Herrmann
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - D. Brus
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - A.-P. Hyvärinen
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - F. Stratmann
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - M. Wilck
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - H. Lihavainen
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
| | - M. Kulmala
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic, Leibniz-Institut für Troposphärenforschung, Leipzig, Germany, and Particle Dynamics GmbH, Leipzig, Germany
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23
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Sipila M, Berndt T, Petaja T, Brus D, Vanhanen J, Stratmann F, Patokoski J, Mauldin RL, Hyvarinen AP, Lihavainen H, Kulmala M. The Role of Sulfuric Acid in Atmospheric Nucleation. Science 2010; 327:1243-6. [DOI: 10.1126/science.1180315] [Citation(s) in RCA: 582] [Impact Index Per Article: 41.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
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Jimenez JL, Canagaratna MR, Donahue NM, Prevot ASH, Zhang Q, Kroll JH, DeCarlo PF, Allan JD, Coe H, Ng NL, Aiken AC, Docherty KS, Ulbrich IM, Grieshop AP, Robinson AL, Duplissy J, Smith JD, Wilson KR, Lanz VA, Hueglin C, Sun YL, Tian J, Laaksonen A, Raatikainen T, Rautiainen J, Vaattovaara P, Ehn M, Kulmala M, Tomlinson JM, Collins DR, Cubison MJ, Dunlea EJ, Huffman JA, Onasch TB, Alfarra MR, Williams PI, Bower K, Kondo Y, Schneider J, Drewnick F, Borrmann S, Weimer S, Demerjian K, Salcedo D, Cottrell L, Griffin R, Takami A, Miyoshi T, Hatakeyama S, Shimono A, Sun JY, Zhang YM, Dzepina K, Kimmel JR, Sueper D, Jayne JT, Herndon SC, Trimborn AM, Williams LR, Wood EC, Middlebrook AM, Kolb CE, Baltensperger U, Worsnop DR. Evolution of Organic Aerosols in the Atmosphere. Science 2009; 326:1525-9. [PMID: 20007897 DOI: 10.1126/science.1180353] [Citation(s) in RCA: 1053] [Impact Index Per Article: 70.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
Affiliation(s)
- J L Jimenez
- Cooperative Institute for Research in the Environmental Sciences and Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA.
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Nieminen T, Manninen HE, Sihto SL, Yli-Juuti T, Mauldin RL, Petäjä T, Riipinen I, Kerminen VM, Kulmala M. Connection of sulfuric acid to atmospheric nucleation in boreal forest. Environ Sci Technol 2009; 43:4715-4721. [PMID: 19673256 DOI: 10.1021/es803152j] [Citation(s) in RCA: 13] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
Gas to particle conversion in the boundary layer occurs worldwide. Sulfuric acid is considered to be one of the key components in these new particle formation events. In this study we explore the connection between measured sulfuric acid and observed formation rate of both charged 2 nm as well as neutral clusters in a boreal forest environment A very short time delay of the order of ten minutes between these two parameters was detected. On average the event days were clearly associated with higher sulfuric acid concentrations and lower condensation sink (CS) values than the nonevent days. Although there was not a clear sharp boundary between the nucleation and no-nucleation days in sulfuric acid-CS plane, at our measurement site a typical threshold concentration of 3.10(5) molecules cm(-3) of sulfuric acid was needed to initiate the new particle formation. Two proposed nucleation mechanisms were tested. Our results are somewhat more in favor of activation type nucleation than of kinetic type nucleation, even though our data set is too limited to omit either of these two mechanisms. In line with earlier studies, the atmospheric nucleation seems to start from sizes very close to 2 nm.
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Affiliation(s)
- T Nieminen
- Department of Physics, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
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26
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Merikanto J, Napari I, Vehkamäki H, Anttila T, Kulmala M. Correction to “New parameterization of sulfuric acid-ammonia-water ternary nucleation rates at tropospheric conditions”. ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2009jd012136] [Citation(s) in RCA: 9] [Impact Index Per Article: 0.6] [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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27
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Grönholm T, Launiainen S, Ahlm L, Mårtensson EM, Kulmala M, Vesala T, Nilsson ED. Aerosol particle dry deposition to canopy and forest floor measured by two-layer eddy covariance system. ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2008jd010663] [Citation(s) in RCA: 25] [Impact Index Per Article: 1.7] [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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28
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Herrmann E, Hyvärinen AP, Brus D, Lihavainen H, Kulmala M. Re-evaluation of the Pressure Effect for Nucleation in Laminar Flow Diffusion Chamber Experiments with Fluent and the Fine Particle Model. J Phys Chem A 2009; 113:1434-9. [DOI: 10.1021/jp809134r] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/07/2023]
Affiliation(s)
- E. Herrmann
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, and Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic
| | - A.-P. Hyvärinen
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, and Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic
| | - D. Brus
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, and Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic
| | - H. Lihavainen
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, and Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic
| | - M. Kulmala
- Department of Physics, University of Helsinki, Finland, Finnish Meteorological Institute, Helsinki, Finland, and Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals ASCR, Prague, Czech Republic
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Vuollekoski H, Kerminen VM, Anttila T, Sihto SL, Vana M, Ehn M, Korhonen H, McFiggans G, O'Dowd CD, Kulmala M. Iodine dioxide nucleation simulations in coastal and remote marine environments. ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2008jd010713] [Citation(s) in RCA: 25] [Impact Index Per Article: 1.7] [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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Bonn B, Kulmala M, Riipinen I, Sihto SL, Ruuskanen TM. How biogenic terpenes govern the correlation between sulfuric acid concentrations and new particle formation. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2007jd009327] [Citation(s) in RCA: 64] [Impact Index Per Article: 4.0] [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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31
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Brus D, Hyvärinen AP, Wedekind J, Viisanen Y, Kulmala M, Ždímal V, Smolík J, Lihavainen H. The homogeneous nucleation of 1-pentanol in a laminar flow diffusion chamber: The effect of pressure and kind of carrier gas. J Chem Phys 2008; 128:134312. [DOI: 10.1063/1.2901049] [Citation(s) in RCA: 12] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/11/2023] Open
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Winkler PM, Steiner G, Vrtala A, Vehkamaki H, Noppel M, Lehtinen KEJ, Reischl GP, Wagner PE, Kulmala M. Heterogeneous Nucleation Experiments Bridging the Scale from Molecular Ion Clusters to Nanoparticles. Science 2008; 319:1374-7. [DOI: 10.1126/science.1149034] [Citation(s) in RCA: 206] [Impact Index Per Article: 12.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
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Abstract
BACKGROUND There is little previous information of the effects of size fractioned particulate air pollution and source specific fine particles (PM(2.5); <2.5 microm) on asthma and chronic obstructive pulmonary disease (COPD) among children, adults and the elderly. OBJECTIVES To determine the effects of daily variation in levels of different particle size fractions and gaseous pollutants on asthma and COPD by age group. METHODS Levels of particulate air pollution, NO(2) and CO were measured from 1998 to 2004 at central outdoor monitoring sites in Helsinki, Finland. Associations between daily pollution levels and hospital emergency room visits were evaluated for asthma (ICD10: J45+J46) in children <15 years old, and for asthma and COPD (ICD10: J41+J44) in adults (15-64 years) and the elderly (>or=65 years). RESULTS Three to 5 day lagged increases in asthma visits were found among children in association with nucleation (<0.03 microm), Aitken (0.03-0.1 microm) and accumulation (0.1-0.29 microm) mode particles, gaseous pollutants and traffic related PM(2.5) (7.8% (95% CI 3.5 to 12.3) for 1.1 microg/m(3) increase in traffic related PM(2.5) at lag 4). Pooled asthma-COPD visits among the elderly were associated with lag 0 of PM(2.5), coarse particles, gaseous pollutants and long range transported and traffic related PM(2.5) (3.9% (95% CI 0.28 to 7.7) at lag 0). Only accumulation mode and coarse particles were associated with asthma and COPD among adults. CONCLUSIONS Among children, traffic related PM(2.5) had delayed effects, whereas among the elderly, several types of particles had effects that were more immediate. These findings suggest that the mechanisms of the respiratory effects of air pollution, and responsible pollutants, differ by age group.
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Affiliation(s)
- J I Halonen
- National Public Health Institute (KTL), Environmental Epidemiology Unit, PO Box 95, FIN-70701 Kuopio, Finland.
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34
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Kourtchev I, Ruuskanen TM, Keronen P, Sogacheva L, Dal Maso M, Reissell A, Chi X, Vermeylen R, Kulmala M, Maenhaut W, Claeys M. Determination of isoprene and alpha-/beta-pinene oxidation products in boreal forest aerosols from Hyytiälä, Finland: diel variations and possible link with particle formation events. Plant Biol (Stuttg) 2008; 10:138-149. [PMID: 18211553 DOI: 10.1055/s-2007-964945] [Citation(s) in RCA: 16] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/25/2023]
Abstract
Biogenic volatile organic compounds (VOCs), such as isoprene and alpha-/beta-pinene, are photo-oxidized in the atmosphere to non-volatile species resulting in secondary organic aerosol (SOA). The goal of this study was to examine time trends and diel variations of oxidation products of isoprene and alpha-/beta-pinene in order to investigate whether they are linked with meteorological parameters or trace gases. Separate day-night aerosol samples (PM(1)) were collected in a Scots pine dominated forest in southern Finland during 28 July-11 August 2005 and analyzed with gas chromatography/mass spectrometry (GC/MS). In addition, inorganic trace gases (SO(2), CO, NO(x), and O(3)), meteorological parameters, and the particle number concentration were monitored. The median total concentration of terpenoic acids (i.e., pinic acid, norpinic acid, and two novel compounds, 3-hydroxyglutaric acid and 2-hydroxy-4-isopropyladipic acid) was 65 ng m(-3), while that of isoprene oxidation products (i.e., 2-methyltetrols and C(5) alkene triols) was 17.2 ng m(-3). The 2-methyltetrols exhibited day/night variations with maxima during day-time, while alpha-/beta-pinene oxidation products did not show any diel variation. The sampling period was marked by a relatively high condensation sink, caused by pre-existing aerosol particles, and no nucleation events. In general, the concentration trends of the SOA compounds reflected those of the inorganic trace gases, meteorological parameters, and condensation sink. Both the isoprene and alpha-/beta-pinene SOA products were strongly influenced by SO(2), which is consistent with earlier reports that acidity plays a role in SOA formation. The results support previous proposals that oxygenated VOCs contribute to particle growth processes above boreal forest.
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Affiliation(s)
- I Kourtchev
- Department of Pharmaceutical Sciences, University of Antwerp (Campus Drie Eiken), Universiteitsplein 1, 2610 Antwerp, Belgium.
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Hienola AI, Winkler PM, Wagner PE, Vehkamäki H, Lauri A, Napari I, Kulmala M. Estimation of line tension and contact angle from heterogeneous nucleation experimental data. J Chem Phys 2007; 126:094705. [PMID: 17362116 DOI: 10.1063/1.2565769] [Citation(s) in RCA: 72] [Impact Index Per Article: 4.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
Abstract
Using the classical nucleation theory corrected with line tension and experimental data of heterogeneous nucleation of n-nonane, n-propanol, and their mixture on silver particles of three different sizes, the authors were able to estimate the line tensions and the microscopic contact angles for the above mentioned systems. To do this they applied generalized Young's equation for the line tension and calculated the interfacial tensions using Li and Neumann's equation [Adv. Colloid Interface Sci. 39, 299 (1992)]. It has been found that, for both unary and binary systems, the line tension is negative and the resulting microscopic contact angle derived from experimental nucleation data is most of the time larger than the macroscopic one. This is in contrast to earlier studies where the influence of line tension has not been accounted for. The values of the three phase contact line tension obtained in this way are of the same order of magnitude as the estimations for other systems reported in literature. The line tension effect also decreases considerably the nucleation barrier.
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Affiliation(s)
- A I Hienola
- Department of Physical Sciences, University of Helsinki, Gustaf Hällströmin katu 2, FIN-00014, Helsinki, Finland
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36
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Merikanto J, Napari I, Vehkamäki H, Anttila T, Kulmala M. New parameterization of sulfuric acid-ammonia-water ternary nucleation rates at tropospheric conditions. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd007977] [Citation(s) in RCA: 115] [Impact Index Per Article: 6.8] [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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37
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Pryor SC, Larsen SE, Sørensen LL, Barthelmie RJ, Grönholm T, Kulmala M, Launiainen S, Rannik Ü, Vesala T. Particle fluxes over forests: Analyses of flux methods and functional dependencies. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd008066] [Citation(s) in RCA: 43] [Impact Index Per Article: 2.5] [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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Abstract
We present experimental results obtained with a differential scanning calorimeter (DSC) that indicate the small ice particles in low-temperature cirrus clouds are not completely solid but rather coated with an unfrozen H2SO4/H2O overlayer. Our results provide a new look on the formation, development, and microphysical properties of low-temperature cirrus clouds.
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Winkler PM, Vrtala A, Rudolf R, Wagner PE, Riipinen I, Vesala T, Lehtinen KEJ, Viisanen Y, Kulmala M. Condensation of water vapor: Experimental determination of mass and thermal accommodation coefficients. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2006jd007194] [Citation(s) in RCA: 67] [Impact Index Per Article: 3.7] [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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40
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Lanki T, Pekkanen J, Aalto P, Elosua R, Berglind N, D'Ippoliti D, Kulmala M, Nyberg F, Peters A, Picciotto S, Salomaa V, Sunyer J, Tiittanen P, von Klot S, Forastiere F. Associations of traffic related air pollutants with hospitalisation for first acute myocardial infarction: the HEAPSS study. Occup Environ Med 2006; 63:844-51. [PMID: 16912091 PMCID: PMC2078003 DOI: 10.1136/oem.2005.023911] [Citation(s) in RCA: 111] [Impact Index Per Article: 6.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/04/2022]
Abstract
BACKGROUND Acute myocardial infarction (AMI) is the leading cause of death attributed to cardiovascular diseases. An association between traffic related air pollution and AMI has been suggested, but the evidence is still limited. OBJECTIVES To evaluate in a multicentre study association between hospitalisation for first AMI and daily levels of traffic related air pollution. METHODS The authors collected data on first AMI hospitalisations in five European cities. AMI registers were available in Augsburg and Barcelona; hospital discharge registers (HDRs) were used in Helsinki, Rome and Stockholm. NO2, CO, PM10 (particles <10 microm), and O3 were measured at central monitoring sites. Particle number concentration (PNC), a proxy for ultrafine particles (<0.1 microm), was measured for a year in each centre, and then modelled retrospectively for the whole study period. Generalised additive models were used for statistical analyses. Age and 28 day fatality and season were considered as potential effect modifiers in the three HDR centres. RESULTS Nearly 27,000 cases of first AMI were recorded. There was a suggestion of an association of the same day CO and PNC levels with AMI: RR = 1.005 (95% CI 1.000 to 1.010) per 0.2 mg/m3 and RR = 1.005 (95% CI 0.996 to 1.015) per 10000 particles/cm3, respectively. However, associations were only observed in the three cities with HDR, where power for city-specific analyses was higher. The authors observed in these cities the most consistent associations among fatal cases aged <75 years: RR at 1 day lag for CO = 1.021 (95% CI 1.000 to 1.048) per 0.2 mg/m3, for PNC = 1.058 (95% CI 1.012 to 1.107) per 10000 particles/cm3, and for NO2 = 1.032 (95% CI 0.998 to 1.066) per 8 microg/m3. Effects of air pollution were more pronounced during the warm than the cold season. CONCLUSIONS The authors found support for the hypothesis that exposure to traffic related air pollution increases the risk of AMI. Most consistent associations were observed among fatal cases aged <75 years and in the warm season.
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Affiliation(s)
- T Lanki
- Environmental Epidemiology Unit, National Public Health Institute (KTL), Kuopio, Finland.
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Tunved P, Hansson HC, Kerminen VM, Ström J, Maso MD, Lihavainen H, Viisanen Y, Aalto PP, Komppula M, Kulmala M. High Natural Aerosol Loading over Boreal Forests. Science 2006; 312:261-3. [PMID: 16614221 DOI: 10.1126/science.1123052] [Citation(s) in RCA: 363] [Impact Index Per Article: 20.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Aerosols play a key role in the radiation balance of the atmosphere. Here, we present evidence that the European boreal region is a substantial source of both aerosol mass and aerosol number. The investigation supplies a straightforward relation between emissions of monoterpenes and gas-to-particle formation over regions substantially lacking in anthropogenic aerosol sources. Our results show that the forest provides an aerosol population of 1000 to 2000 particles of climatically active sizes per cubic centimeter during the late spring to early fall period. This has important implications for radiation budget estimates and relevancy for the evaluation of feedback loops believed to determine our future climate.
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Affiliation(s)
- P Tunved
- Department of Applied Environmental Science (ITM), Air Pollution Laboratory, Frescativägen 54, SE-106 91, Stockholm, Sweden.
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Gaman AI, Napari I, Winkler PM, Vehkamäki H, Wagner PE, Strey R, Viisanen Y, Kulmala M. Homogeneous nucleation of n-nonane and n-propanol mixtures: A comparison of classical nucleation theory and experiments. J Chem Phys 2005; 123:244502. [PMID: 16396544 DOI: 10.1063/1.2138703] [Citation(s) in RCA: 19] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
Abstract
The homogeneous nucleation rates for n-nonane-n-propanol vapor mixtures have been calculated as a function of vapor-phase activities at 230 K using the classical nucleation theory (CNT) with both rigorous and approximate kinetic prefactors and compared to previously reported experimental data. The predicted nucleation rates resemble qualitatively the experimental results for low n-nonane gas phase activity. On the high nonane activity side the theoretical nucleation rates are about three orders of magnitude lower than the experimental data when using the CNT with the approximate kinetics. The accurate kinetics improves the situation by reducing the difference between theory and experiments to two orders of magnitude. Besides the nucleation rate comparison and the experimental and predicted onset activities, the critical cluster composition is presented. The total number of molecules is approximated by CNT with reasonable accuracy. Overall, the classical nucleation theory with rigorous kinetic prefactor seems to perform better. The thermodynamic parameters needed to calculate the nucleation rates are revised extensively. Up-to-date estimates of liquid phase activities using universal functional activity coefficient Dortmund method are presented together with the experimental values of surface tensions obtained in the present study.
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Affiliation(s)
- A I Gaman
- Department of Physical Sciences, University of Helsinki, 00014 Helsinki, Finland.
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43
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Mönkkönen P, Pai P, Maynard A, Lehtinen KEJ, Hämeri K, Rechkemmer P, Ramachandran G, Prasad B, Kulmala M. Fine particle number and mass concentration measurements in urban Indian households. Sci Total Environ 2005; 347:131-47. [PMID: 16084974 DOI: 10.1016/j.scitotenv.2004.12.023] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/22/2004] [Accepted: 12/17/2004] [Indexed: 05/03/2023]
Abstract
Fine particle number concentration (D(p)>10 nm, cm(-3)), mass concentrations (approximation of PM(2.5), microg m(-3)) and indoor/outdoor number concentration ratio (I/O) measurements have been conducted for the first time in 11 urban households in India, 2002. The results indicate remarkable high indoor number and mass concentrations and I/O number concentration ratios caused by cooking. Besides cooking stoves that used liquefied petroleum gas (LPG) or kerosene as the main fuel, high indoor concentrations can be explained by poor ventilation systems. Particle number concentrations of more than 300,000 cm(-3) and mass concentrations of more than 1000 microg m(-3) were detected in some cases. When the number and mass concentrations during cooking times were statistically compared, a correlation coefficient r>0.50 was observed in 63% of the households. Some households used other fuels like wood and dung cakes along with the main fuel, but also other living activities influenced the concentrations. In some areas, outdoor combustion processes had a negative impact on indoor air quality. The maximum concentrations observed in most cases were due to indoor combustion sources. Reduction of exposure risk and health effects caused by poor indoor air in urban Indian households is possible by improving indoor ventilation and reducing penetration of outdoor particles.
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Affiliation(s)
- P Mönkkönen
- University of Helsinki, Department of Physical Sciences, P.O. Box 64, 00014 Helsinki, Finland.
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Tervahattu H, Juhanoja J, Vaida V, Tuck AF, Niemi JV, Kupiainen K, Kulmala M, Vehkamäki H. Fatty acids on continental sulfate aerosol particles. ACTA ACUST UNITED AC 2005. [DOI: 10.1029/2004jd005400] [Citation(s) in RCA: 95] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- H. Tervahattu
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
| | | | - V. Vaida
- Department of Chemistry and Biochemistry; University of Colorado; Boulder Colorado USA
| | - A. F. Tuck
- Aeronomy Laboratory; National Oceanic and Atmospheric Administration; Boulder Colorado USA
| | - J. V. Niemi
- Department of Biological and Environmental Sciences; University of Helsinki; Helsinki Finland
| | - K. Kupiainen
- Department of Biological and Environmental Sciences; University of Helsinki; Helsinki Finland
- Nordic Envicon Oy; Helsinki Finland
| | - M. Kulmala
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - H. Vehkamäki
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
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Lehtinen KEJ, Rannik Ü, Petäjä T, Kulmala M, Hari P. Nucleation rate and vapor concentration estimations using a least squares aerosol dynamics method. ACTA ACUST UNITED AC 2004. [DOI: 10.1029/2004jd004893] [Citation(s) in RCA: 12] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- K. E. J. Lehtinen
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - Ü. Rannik
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - T. Petäjä
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - M. Kulmala
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - P. Hari
- Department of Forest Ecology; University of Helsinki; Helsinki Finland
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Lushnikov AA, Kulmala M. Flux-matching theory of particle charging. Phys Rev E Stat Nonlin Soft Matter Phys 2004; 70:046413. [PMID: 15600536 DOI: 10.1103/physreve.70.046413] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/30/2004] [Revised: 06/01/2004] [Indexed: 05/24/2023]
Abstract
A new flux-matching theory is formulated and applied to the study of particle charging by ions. Assuming that the ion-particle interaction includes the Coulomb + polarization forces the collisionless kinetic equation is solved and the ion concentration profile in the free-molecule zone (at the distances less than the ion mean free path) is found. This profile is then matched to that derived from the solution of the diffusion equation, which describes the ion transport outside the free-molecule zone. Three matching parameters are introduced: the ion flux, the matching distance, and the ion density at the matching distance; and three conditions are formulated for fixing these parameters: (i) the constancy of the total ion flux, (ii) the continuity of the ion concentration profile, and (iii) the continuity of the derivative of the ion concentration profile. The charging efficiencies are expressed in terms of their free-molecule values, the ion diffusivity in the carrier gas, and the ion thermal velocity. This approach is applied for calculating the efficiencies of particle charging in the transition regime (the particle size is comparable to the ion mean free path and the Coulomb length). The corrections due to ion-carrier gas interaction to the particle-ion recombination rate are shown to remain finite even for very small particles, whereas in the case of particle-ion repulsion the contribution of ion-molecular collisions to the rate of particle charging is suppressed in the free-molecule regime.
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Affiliation(s)
- A A Lushnikov
- Department of Physical Sciences, University of Helsinki, P.O. Box 64, FIN-00014, Helsinki, Finland
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Lihavainen H, Kerminen VM, Komppula M, Hatakka J, Aaltonen V, Kulmala M, Viisanen Y. Production of “potential” cloud condensation nuclei associated with atmospheric new-particle formation in northern Finland. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2003jd003887] [Citation(s) in RCA: 96] [Impact Index Per Article: 4.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- H. Lihavainen
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - V.-M. Kerminen
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - M. Komppula
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - J. Hatakka
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - V. Aaltonen
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - M. Kulmala
- Division of Atmospheric Sciences, Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - Y. Viisanen
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
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Noppel M, Vehkamäki H, Kulmala M. Reversible work of the formation of a layer of a new phase on a spherical charged conductor within a uniform multicomponent macroscopic mother phase. J Chem Phys 2003. [DOI: 10.1063/1.1620499] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
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Boy M, Rannik Ü, Lehtinen KEJ, Tarvainen V, Hakola H, Kulmala M. Nucleation events in the continental boundary layer: Long-term statistical analyses of aerosol relevant characteristics. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2003jd003838] [Citation(s) in RCA: 52] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- M. Boy
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - Ü. Rannik
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - K. E. J. Lehtinen
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
| | - V. Tarvainen
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - H. Hakola
- Air Quality Research; Finnish Meteorological Institute; Helsinki Finland
| | - M. Kulmala
- Department of Physical Sciences; University of Helsinki; Helsinki Finland
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Vehkamäki H, Kulmala M, Lehtinen KEJ, Noppel M. Modelling binary homogeneous nucleation of water-sulfuric acid vapours: parameterisation for high temperature emissions. Environ Sci Technol 2003; 37:3392-3398. [PMID: 12966986 DOI: 10.1021/es0263442] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/24/2023]
Abstract
Particles formed in the automobile exhaust might form a significant fraction of fine particles in urban air. We have developed a model and produced parametrizations for predicting the particle formation rate at exhaust conditions. We studied the formation in the mixture of water and sulfuric acid vapors and at temperatures between 300 and 400 K. A thermodynamically consistent version of the classical binary homogeneous nucleation model was used. The needed thermodynamical input data (vapor pressures, chemical activities, surface tensions, densities) are carefully investigated and utilized in thermodynamically consistent way. The obtained nucleation rates are parametrized in order to be able to use this nucleation model in aerosol dynamic models, exhaust models, or other process models. The parametrization reduces computational time at least by a factor of 500.
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Affiliation(s)
- H Vehkamäki
- Division of Atmospheric Sciences, Department of Physical Sciences, P.O. Box 64 (Gustaf Hällströmin katu 2) FIN-00014 University of Helsinki, Finland.
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