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Novel insights on new particle formation derived from a pan-european observing system.
Dall'Osto, M; Beddows, D C S; Asmi, A; Poulain, L; Hao, L; Freney, E; Allan, J D; Canagaratna, M; Crippa, M; Bianchi, F; de Leeuw, G; Eriksson, A; Swietlicki, E; Hansson, H C; Henzing, J S; Granier, C; Zemankova, K; Laj, P; Onasch, T; Prevot, A; Putaud, J P; Sellegri, K; Vidal, M; Virtanen, A; Simo, R; Worsnop, D; O'Dowd, C; Kulmala, M; Harrison, Roy M.
Afiliação
  • Dall'Osto M; Institute of Marine Science, Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain. dallosto@icm.csic.es.
  • Beddows DCS; 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. dallosto@icm.csic.es.
  • Asmi A; School of Physics, Centre for Climate & Air Pollution Studies, National University of Ireland Galway, University Road Galway, Galway, Ireland. dallosto@icm.csic.es.
  • Poulain L; Aerodyne Research, Inc., Billerica, MA, USA. dallosto@icm.csic.es.
  • Hao L; 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.
  • Freney E; Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.
  • Allan JD; Leibniz Institute for Tropospheric Research, Permoserstr. 15, 04318, Leipzig, Germany.
  • Canagaratna M; University of Eastern Finland, Department of Applied Physics, P.O.Box 1627, FIN-70211, Kuopio, Finland.
  • Crippa M; Laboratoire de Météorologie Physique, CNRS-Université Blaise Pascal, UMR6016, 63117, Clermont, Ferrand, France.
  • Bianchi F; School of Earth, Atmospheric and Environmental Sciences, The University of Manchester, Manchester, UK.
  • de Leeuw G; Aerodyne Research, Inc., Billerica, MA, USA.
  • Eriksson A; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland.
  • Swietlicki E; 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.
  • Hansson HC; Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.
  • Henzing JS; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland.
  • Granier C; Finnish Meteorological Institute, Climate Change Unit, P.O. Box 503, 00101, Helsinki, Finland.
  • Zemankova K; Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands.
  • Laj P; Division of Ergonomics and Aerosol Technology, Lund University, Box 118, SE-22100, Lund, Sweden.
  • Onasch T; Division of Nuclear Physics, Lund University, Box 118, SE-22100, Lund, Sweden.
  • Prevot A; Department of Environmental Science and Analytical Chemistry, Stockholm University, 10691, Stockholm, Sweden.
  • Putaud JP; Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands.
  • Sellegri K; Laboratoire d'Aérologie, Toulouse, France.
  • Vidal M; NOAA Earth System Laboratory and CIRES, University of Colorado, Boulder, USA.
  • Virtanen A; Charles University, Faculty of Mathematics and Physics, Dept. of Atmospheric Physcis, Prague, Czechia.
  • Simo R; Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.
  • Worsnop D; Univ. Grenoble-Alpes, CNRS, IRD, INPG, Institut des Géosciences de l'Environnement, Grenoble, France.
  • O'Dowd C; Univ. Grenoble-Alpes, CNRS, IRD, Observatoire des Sciences de l'Univers, Grenoble, France.
  • Kulmala M; Aerodyne Research, Inc., Billerica, MA, USA.
  • Harrison RM; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland.
Sci Rep ; 8(1): 1482, 2018 01 24.
Article em En | MEDLINE | ID: mdl-29367716
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.

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Ano de publicação: 2018 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Ano de publicação: 2018 Tipo de documento: Article