Articles | Volume 9, issue 8
https://doi.org/10.5194/gmd-9-2741-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-9-2741-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Development and technical paper
| 
22 Aug 2016
Development and technical paper |
| 22 Aug 2016
Implementation of state-of-the-art ternary new-particle formation scheme to the regional chemical transport model PMCAMx-UF in Europe
Elham Baranizadeh
Aerosol Physics Group, Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Benjamin N. Murphy
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
now at: the National Exposure Research Laboratory, US Environmental Protection Agency, Research Triangle Park, Durham, NC, USA
Jan Julin
Aerosol Physics Group, Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
Saeed Falahat
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
now at: the Swedish Meteorological and Hydrological institute (SMHI), Norrköping, Sweden
Carly L. Reddington
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
Antti Arola
Atmospheric Research Centre of Eastern Finland, Finnish Meteorological Institute, Kuopio, Finland
Lars Ahlm
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
Santtu Mikkonen
Aerosol Physics Group, Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Christos Fountoukis
Qatar Environment and Energy Research Institute (QEERI), Hamad Bin Khalifa University (HBKU), Qatar Foundation, Doha, Qatar
David Patoulias
Department of Chemical Engineering, University of Patras, Patras, Greece
Andreas Minikin
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
now at: Deutsches Zentrum für Luft- und Raumfahrt (DLR), Flugexperimente, Oberpfaffenhofen, Germany
Thomas Hamburger
Atmosphere and Climate Department (ATMOS), Norwegian Institute for Air Research (NILU), Oslo, Norway
now at: Federal Office for Radiation Protection (BfS), Neuherberg, Germany
Ari Laaksonen
Aerosol Physics Group, Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Climate research Unit, Finnish Meteorological Institute, Helsinki, Finland
Spyros N. Pandis
Department of Chemical Engineering, University of Patras, Patras, Greece
Institute of Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICEHT/FORTH), Patras, Greece
Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA
Hanna Vehkamäki
Division of Atmospheric Sciences, Department of Physics, University of Helsinki, Helsinki, Finland
Kari E. J. Lehtinen
Aerosol Physics Group, Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Atmospheric Research Centre of Eastern Finland, Finnish Meteorological Institute, Kuopio, Finland
Ilona Riipinen
CORRESPONDING AUTHOR
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
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Short summary
The molecular mechanisms through which new ultrafine (< 100 nm) aerosol particles are formed in the atmosphere have puzzled the scientific community for decades. In the past few years, however, significant progress has been made in unraveling these processes through laboratory studies and computational efforts. In this work we have implemented these new developments to an air quality model and study the implications of anthropogenically driven particle formation for European air quality.
The molecular mechanisms through which new ultrafine (< 100 nm) aerosol particles are formed in...
