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A modelling study of OH, NO3 and H2SO4 in 2007-2018 at SMEAR II, Finland: analysis of long-term trends.
Chen, Dean; Xavier, Carlton; Clusius, Petri; Nieminen, Tuomo; Roldin, Pontus; Qi, Ximeng; Pichelstorfer, Lukas; Kulmala, Markku; Rantala, Pekka; Aalto, Juho; Sarnela, Nina; Kolari, Pasi; Keronen, Petri; Rissanen, Matti P; Taipale, Ditte; Foreback, Benjamin; Baykara, Metin; Zhou, Putian; Boy, Michael.
Afiliación
  • Chen D; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Xavier C; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Clusius P; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Nieminen T; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Roldin P; Institute for Atmospheric and Earth System Research/Forest Sciences, University of Helsinki P.O. Box 64 00014 Helsinki Finland.
  • Qi X; Division of Nuclear Physics, Department of Physics, Lund University P.O. Box 118 SE-22100 Lund Sweden.
  • Pichelstorfer L; Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University Nanjing 210023 China.
  • Kulmala M; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Rantala P; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Aalto J; Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University Nanjing 210023 China.
  • Sarnela N; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Kolari P; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Keronen P; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Rissanen MP; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Taipale D; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Foreback B; Aerosol Physics Laboratory, Physics Unit, Faculty of Engineering and Natural Sciences, Tampere University Tampere Finland.
  • Baykara M; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Zhou P; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
  • Boy M; Institute for Atmospheric and Earth System Research/Physics, University of Helsinki P.O. Box 64 00014 Helsinki Finland putian.zhou@helsinki.fi.
Environ Sci Atmos ; 1(6): 449-472, 2021 Sep 23.
Article en En | MEDLINE | ID: mdl-34604756
ABSTRACT
Major atmospheric oxidants (OH, O3 and NO3) dominate the atmospheric oxidation capacity, while H2SO4 is considered as a main driver for new particle formation. Although numerous studies have investigated the long-term trend of ozone in Europe, the trends of OH, NO3 and H2SO4 at specific sites are to a large extent unknown. The one-dimensional model SOSAA has been applied in several studies at the SMEAR II station and has been validated by measurements in several projects. Here, we applied the SOSAA model for the years 2007-2018 to simulate the atmospheric chemical components, especially the atmospheric oxidants OH and NO3, as well as H2SO4 at SMEAR II. The simulations were evaluated with observations from several shorter and longer campaigns at SMEAR II. Our results show that daily OH increased by 2.39% per year and NO3 decreased by 3.41% per year, with different trends of these oxidants during day and night. On the contrary, daytime sulfuric acid concentrations decreased by 2.78% per year, which correlated with the observed decreasing concentration of newly formed particles in the size range of 3-25 nm with 1.4% per year at SMEAR II during the years 1997-2012. Additionally, we compared our simulated OH, NO3 and H2SO4 concentrations with proxies, which are commonly applied in case a limited number of parameters are measured and no detailed model simulations are available.

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Environ Sci Atmos Año: 2021 Tipo del documento: Article

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Environ Sci Atmos Año: 2021 Tipo del documento: Article