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Observations of new particle formation events in the south-eastern Baltic Sea

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
New particle formation and growth were observed at a coastal site (Preila station, Lithuania) during 1997 and 2000-2002. The total amount of data analysed covers 291 one-day periods, 45 (15%) of which were long-term, new particle formation days. Short-term nucleation events (from a few minutes to one hour) and long-term events (from one to eight hours) were identified. The mean particle growth rate, condensation sink and condensable vapour source rate during nucleation events were 3.9 nm h*-1, 1.45 × 10*-3 cm*-3 s-1 and 7.5 x 104 cm-3 s-1 respectively. The average formation rate J_10 was 0.4 cm-3 s-1. The nucleation events were accompanied mainly by air masses transported from the north (43%) and north-west (19%). Meteorological parameters and trace gas (O3, SO2, NO2) concentrations were also analysed. It was found that nucleation events are related to high levels of solar radiation.
Czasopismo
Rocznik
Strony
53--75
Opis fizyczny
bibliogr. 45 poz., tab., wykr.
Twórcy
autor
autor
  • Environmental Physics and Chemistry Laboratory, Institute of Physics, Savanoriu 231, LT-02300 Vilnius, Lithuania, ulevicv@ktl.mii.lt
Bibliografia
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  • 19.Kulmala M., Dal Maso M., Mäkelä J.M., Pirjola L., Väkevä M., Aalto P., Miikkulainen P., Hämeri K., O'Dowd C., 2001, On the formation, growth and composition of nucleation mode particles, Tellus B, 53 (4), 479-490.
  • 20.Kulmala M., Kerminen V.-M., Laaksonen A., Riipinen I., Sipilä M., Ruuskanen T.M., Sogatcheva L., Hari P., Bäck J., Lehtinen K.E. J., Viisanen Y., Bilde M., Svenningson B., Lazaridis M., Törseth K., Tunved P., Nilsson D., Pryor S., Sörensen L.-L., Hörrak U., Winkler P.M., Swietlicki E., Riekkola M.-L., Krejci R., Hoyle C., Hovö., Myhre G., Hansson H.-C., 2008, Overview of the biosphere aerosol cloud climate interactions (BACCI) studies, Tellus B, 60 (2), 300-317.
  • 21.Kulmala M., Lehtinen K.E. J., Laaksonen A., 2006, Cluster activation theory as an explanation of the linear dependence between formation rate of 3 nm particles and sulphuric acid concentration, Atmos. Chem. Phys., 6 (3), 787-793.
  • 22.Kulmala M., Pirjola L., Mäkelä J.M., 2000a, Stable sulphate clusters as a source of new atmospheric particles, Nature, 404 (6773), 66-69.
  • 23.Kulmala M., Rannik Ű., Pirjola L., Dal Maso M., Karimäki J., Asmi A., Jäppinen A., Karhu V., Korhonen H., Malvikko S.-P., Puustinen A., Raittile J., Romakkaniemi S., Suni T., Ylikoivisto S., Paatero J., Harri P., Vesala T., 2000b, Characterization of the atmospheric gas and aerosol concentration at forest sites in southern and northern Finland using back trajectories, Boreal Environ. Res., 5 (4), 281-297.
  • 24.Kulmala M., Toivonen A., Mäkelä J.M., Laaksonen A., 1998, Analysis and growth of the nucleation mode particles observed in a Boreal forest, Tellus B, 50 (5), 449-462.
  • 25.Kulmala M., Vehkamäki H., Petäjä T., Dal Maso M., Lauri A., Kerminen V.-M., Birmili W., McMurry P.H., 2004, Formation and growth rates of ultrafine atmospheric particles: a review of observations, J. Aerosol Sci., 35 (2), 143-176.
  • 26.Laakso L., Anttila T., Lehtinen K.E. J., Aalto P.P., Kulmala M., H˜orrak U., Paatero J., Hanke M., Arnold F., 2004, Kinetic nucleation and ions in boreal forest particle formation events, Atmos. Chem. Phys., 4 (9-10), 2353-2366.
  • 27.Lazaridis M., Eleftheriadis K., Smolik J., Colbeck I., Kallos G., Drossinos Y., Zdimal V., Vecera Z., Mihalopoulos N., Mikuska P., Bryant C., Housiadas C., Spyridaki A., Astitha M., Havranek V., 2006, Dynamics of fine particles and photo-oxidants in the Eastern Mediterranean (SUB-AERO), Atmos. Environ., 40 (32), 6214-6228.
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  • 29.Mäkelä J.M., Koponen I.K., Aalto P., Kulmala M., 2000, One-year data of submicron size modes of tropospheric background aerosol in southern Finland, J. Aerosol Sci., 31 (5), 595-611.
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  • 31.Nilsson E.D., Kulmala M., 1998, The potential for atmospheric mixing processes to enhance the binary nucleation rate, J. Geophys. Res., 103 (D1), 1381-1389.
  • 32.Nilsson E.D., Paatero J., Boy M., 2001, Effects of air masses and synoptic weather on aerosol formation in the continental boundary layer, Tellus B, 53 (4), 462-478.
  • 33.O'Dowd C.D., Becker E., Kulmala M., 2001, Mid-latitude North-Atlantic aerosol characteristics in clean and polluted air, Atmos. Res., 58 (3), 167-185.
  • 34.O'Dowd C.D., Hämeri K., Mäkelä J.M., Pirjola L., Kulmala M., Jennings S.G., Berresheim H., Hansson H.-C., de Leeuw G., Kunz G. J., Allen A.G., Hewitt C.N., Jackson A., Viisanen Y., Hoffmann T., 2002, A dedicated study of new particle formation and fate in the coastal environment (PARFORCE); Overview of objectives and achievements, J. Geophys. Res., 107 (D19), 8108, doi:10.1029/2001JD000555.
  • 35.Plauškaitė K., 2008, Aerosol particle formation and growth in the marine, coastal and continental environments, Ph.D. thesis, Univ. Vilnius, Inst. Phys., Vilnius, Lithuania.
  • 36.Plauškaitė K., Gaman A., Lehtinen K.E. J., Mordas G., Ulevicius V., Kulmala M., 2003, A comparison study of meteorological parameters, trace gases and nucleation events in Preila and Hyytiälä, Environ. Chem. Phys., 25 (2), 60-69.
  • 37.Plauškaitė K., Kazlauskaitė R., Andriejauskienė J., Ulevicius V., 2005, Parameterization of new particle formation and growth at the Preila station, Lith. J. Phys., 45 (2), 139-147.
  • 38.Pugatshova A., Reinart A., Tamm E., 2007, Features of the multimodal aerosol size distribution depending on the air mass origin in the Baltic region, Atmos. Environ., 41 (21), 4408-4422.
  • 39.Shiobara M., Hara K., Yabuki M., Kobayashi H., 2007, Optical and chemical properties of marine boundary-layer aerosol around Japan determined from shipboard measurements in 2002, Atmos. Environ., 41 (22), 4638-4652.
  • 40.Sihto S.-L., Kulmala M., Kerminen V.-M., Dal Maso M., Petäjä T., Riipinen I., Korhonen H., Arnold F., Janson R., Boy M., Laaksonen A., Lehtinen K.E. J., 2006, Atmospheric sulphuric acid and aerosol formation: Implications from atmospheric measurements for nucleation and early growth mechanisms, Atmos. Chem. Phys., 6 (12), 4079-4091.
  • 41.Sogacheva L., Dal Maso M., Kerminen V.-M., Kulmala M., 2005, Probability of nucleation events and aerosol particle concentration in different air mass types arriving at Hyytiälä, southern Finland, based on back trajectories analysis, Boreal Environ. Res., 10 (6), 479-491.
  • 42.Ulevicius V., Mordas G., Plauškaitė K., 2002, Nucleation events at the Preila environmental research station, Environ. Chem. Phys., 24 (2), 38-44.
  • 43.Weber R. J., McMurry P.H., Mauldin L., Tanner D. J., Eisele F. L., Brechtel F. J., Kreidenweis S.M., Kok G. L., Schillawski R.D., Baumgardner D., 1998, A study of new particle formation and growth involving biogenic and trace gas species measured during ACE 1, J. Geophys. Res., 103 (D13), 16 385-16 396.
  • 44.Wehner B., Siebert H., Stratmann F., Tuch T., Wiedensohler A., Petäjä T., Dal Maso M., Kulmala M., 2007, Horizontal homogeneity and vertical extent of new particle formation events, Tellus B, 59 (3), 362-371.
  • 45.Xie Z., Sun L., Blum J.D., Huang Y., He W., 2006, Summertime aerosol chemical components in the marine boundary layer of the Arctic Ocean, J. Geophys. Res., 111, D10309, doi:10.1029/2005JD006777.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0020-0051
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