Hasil Pencarian - M. Kulmala

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  1. 1
    Exploring the potential of nano-Köhler theory to describe the growth of atmospheric molecular clusters by organic vapors using cluster kinetics simulations

    Exploring the potential of nano-Köhler theory to describe the growth of atmospheric molecular clusters by organic vapors using cluster kinetics simulations oleh J. Kontkanen, J. Kontkanen, T. Olenius, M. Kulmala, M. Kulmala, M. Kulmala, I. Riipinen

    Diterbitkan 2018-09-01
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  2. 2
    Estimation of sulfuric acid concentration using ambient ion composition and concentration data obtained with atmospheric pressure interface time-of-flight ion mass spectrometer

    Estimation of sulfuric acid concentration using ambient ion composition and concentration data obtained with atmospheric pressure interface time-of-flight ion mass spectrometer oleh L. J. Beck, S. Schobesberger, M. Sipilä, V.-M. Kerminen, V.-M. Kerminen, M. Kulmala, M. Kulmala, M. Kulmala

    Diterbitkan 2022-03-01
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  3. 3
    Comprehensive analysis of particle growth rates from nucleation mode to cloud condensation nuclei in boreal forest

    Comprehensive analysis of particle growth rates from nucleation mode to cloud condensation nuclei in boreal forest oleh P. Paasonen, M. Peltola, J. Kontkanen, H. Junninen, H. Junninen, V.-M. Kerminen, M. Kulmala, M. Kulmala, M. Kulmala

    Diterbitkan 2018-08-01
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  4. 4
    Pushing nano-aerosol measurements towards a new decade – technical note on the Airmodus particle size magnifier 2.0

    Pushing nano-aerosol measurements towards a new decade – technical note on the Airmodus particle size magnifier 2.0 oleh J. Sulo, J. Enroth, A. Pajunoja, J. Vanhanen, K. Lehtipalo, K. Lehtipalo, T. Petäjä, M. Kulmala, M. Kulmala, M. Kulmala

    Diterbitkan 2024-02-01
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  5. 5
    Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century

    Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century oleh M. Bister, M. Kulmala

    Diterbitkan 2011-05-01
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  6. 6
    The part of the solar spectrum with the highest influence on the formation of SOA in the continental boundary layer

    The part of the solar spectrum with the highest influence on the formation of SOA in the continental boundary layer oleh M. Boy, M. Kulmala

    Diterbitkan 2002-01-01
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  7. 7
    Nucleation events in the continental boundary layer: Influence of physical and meteorological parameters

    Nucleation events in the continental boundary layer: Influence of physical and meteorological parameters oleh M. Boy, M. Kulmala

    Diterbitkan 2002-01-01
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  8. 8
    On the relation between apparent ion and total particle growth rates in the boreal forest and related chamber experiments

    On the relation between apparent ion and total particle growth rates in the boreal forest and related chamber experiments oleh L. Gonzalez Carracedo, K. Lehtipalo, K. Lehtipalo, L. R. Ahonen, N. Sarnela, S. Holm, J. Kangasluoma, M. Kulmala, M. Kulmala, M. Kulmala, M. Kulmala, P. M. Winkler, D. Stolzenburg

    Diterbitkan 2022-10-01
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  9. 9
    Opinion: Gigacity – a source of problems or the new way to sustainable development

    Opinion: Gigacity – a source of problems or the new way to sustainable development oleh M. Kulmala, M. Kulmala, M. Kulmala, T. V. Kokkonen, T. V. Kokkonen, J. Pekkanen, J. Pekkanen, S. Paatero, T. Petäjä, T. Petäjä, T. Petäjä, V.-M. Kerminen, A. Ding

    Diterbitkan 2021-05-01
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  10. 10
    Delineation of dew formation zones in Iran using long-term model simulations and cluster analysis

    Delineation of dew formation zones in Iran using long-term model simulations and cluster analysis oleh N. Atashi, N. Atashi, D. Rahimi, V. A. Sinclair, M. A. Zaidan, M. A. Zaidan, A. Rusanen, H. Vuollekoski, M. Kulmala, M. Kulmala, M. Kulmala, M. Kulmala, T. Vesala, T. Vesala, T. Vesala, T. Hussein, T. Hussein

    Diterbitkan 2021-08-01
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  11. 11
    SMEARcore – modular data infrastructure for atmospheric measurement stations

    SMEARcore – modular data infrastructure for atmospheric measurement stations oleh A. Rusanen, K. Hõrrak, L. R. Ahonen, T. Nieminen, T. Nieminen, P. P. Aalto, P. Kolari, M. Kulmala, M. Kulmala, M. Kulmala, T. Petäjä, T. Petäjä, H. Junninen

    Diterbitkan 2023-06-01
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  12. 12
    Dynamics of aerosol, humidity, and clouds in air masses travelling over Fennoscandian boreal forests

    Dynamics of aerosol, humidity, and clouds in air masses travelling over Fennoscandian boreal forests oleh M. Räty, L. Sogacheva, H.-M. Keskinen, H.-M. Keskinen, V.-M. Kerminen, T. Nieminen, T. Nieminen, T. Petäjä, T. Petäjä, E. Ezhova, M. Kulmala, M. Kulmala, M. Kulmala

    Diterbitkan 2023-03-01
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  13. 13
    On the potential of the Cluster Ion Counter (CIC) to observe local new particle formation, condensation sink and growth rate of newly formed particles

    On the potential of the Cluster Ion Counter (CIC) to observe local new particle formation, condensation sink and growth rate of newly formed particles oleh M. Kulmala, M. Kulmala, M. Kulmala, S. Tuovinen, S. Mirme, S. Mirme, P. Koemets, P. Koemets, L. Ahonen, Y. Liu, H. Junninen, T. Petäjä, T. Petäjä, T. Petäjä, V.-M. Kerminen

    Diterbitkan 2024-10-01
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  14. 14
    A model for particle formation and growth in the atmosphere with molecular resolution in size

    A model for particle formation and growth in the atmosphere with molecular resolution in size oleh K. E. J. Lehtinen, M. Kulmala

    Diterbitkan 2003-01-01
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  15. 15
    Negatively charged nanoparticles produced by splashing of water

    Negatively charged nanoparticles produced by splashing of water oleh H. Tammet, U. Hõrrak, M. Kulmala

    Diterbitkan 2009-01-01
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  16. 16
    Atmospheric new particle formation in China

    Atmospheric new particle formation in China oleh B. Chu, V.-M. Kerminen, F. Bianchi, F. Bianchi, C. Yan, T. Petäjä, T. Petäjä, M. Kulmala, M. Kulmala

    Diterbitkan 2019-01-01
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  17. 17
    Amines are likely to enhance neutral and ion-induced sulfuric acid-water nucleation in the atmosphere more effectively than ammonia

    Amines are likely to enhance neutral and ion-induced sulfuric acid-water nucleation in the atmosphere more effectively than ammonia oleh T. Kurtén, V. Loukonen, H. Vehkamäki, M. Kulmala

    Diterbitkan 2008-07-01
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  18. 18
    Modelling Ag-particle activation and growth in a TSI WCPC model 3785

    Modelling Ag-particle activation and growth in a TSI WCPC model 3785 oleh F. Stratmann, E. Herrmann, T. Petäjä, M. Kulmala

    Diterbitkan 2010-02-01
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  19. 19
    Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed

    Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed oleh T. Nieminen, K. E. J. Lehtinen, M. Kulmala

    Diterbitkan 2010-10-01
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  20. 20
    The effectiveness of the coagulation sink of 3–10 nm atmospheric particles

    The effectiveness of the coagulation sink of 3–10 nm atmospheric particles oleh R. Cai, E. Häkkinen, C. Yan, C. Yan, J. Jiang, M. Kulmala, M. Kulmala, J. Kangasluoma, J. Kangasluoma

    Diterbitkan 2022-09-01
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