Browsing by Author "Dupuy, R."

Now showing items 1-3 of 3

    • Aerosol properties associated with air masses arriving into the north east atlantic during the 2008 mace head eucaari intensive observing period: an overview 

      Dall'Osto, M.; Ceburnis, D.; Martucci, G.; Bialek, J.; Dupuy, R.; Jennings, S. G.; Berresheim, H.; Wenger, J.; Healy, R.; Facchini, M. C.; Rinaldi, M.; Giulianelli, L.; Finessi, E.; Worsnop, D.; Ehn, M.; Mikkilä, J.; Kulmala, M.; O'Dowd, C. D. (Copernicus GmbH, 2010-09-07)
      As part of the EUCAARI Intensive Observing Period, a 4-week campaign to measure aerosol physical, chemical and optical properties, atmospheric structure, and cloud microphysics was conducted from mid-May to mid-June, 2008 ...

    • Nanoparticles in boreal forest and coastal environment: a comparison of observations and implications of the nucleation mechanism 

      Lehtipalo, K.; Kulmala, M.; Sipilä, M.; Petäjä, T.; Vana, M.; Ceburnis, D.; Dupuy, R.; O'Dowd, C. (Copernicus GmbH, 2010-08-02)
      The detailed mechanism of secondary new particle formation in the atmosphere is still under debate. It is proposed that particle formation happens via activation of 1-2 nm atmospheric neutral molecular clusters and/or large ...

    • Primary versus secondary contributions to particle number concentrations in the european boundary layer 

      Reddington, C. L.; Carslaw, K. S.; Spracklen, D. V.; Frontoso, M. G.; Collins, L.; Merikanto, J.; Minikin, A.; Hamburger, T.; Coe, H.; Kulmala, M.; Aalto, P.; Flentje, H.; Plass-Dülmer, C.; Birmili, W.; Wiedensohler, A.; Wehner, B.; Tuch, T.; Sonntag, A.; O'Dowd, C. D.; Jennings, S. G.; Dupuy, R.; Baltensperger, U.; Weingartner, E.; Hansson, H.-C.; Tunved, P.; Laj, P.; Sellegri, K.; Boulon, J.; Putaud, J.-P.; Gruening, C.; Swietlicki, E.; Roldin, P.; Henzing, J. S.; Moerman, M.; Mihalopoulos, N.; Kouvarakis, G.; Ždímal, V.; Zíková, N.; Marinoni, A.; Bonasoni, P.; Duchi, R. (Copernicus GmbH, 2011-12-05)
      It is important to understand the relative contribution of primary and secondary particles to regional and global aerosol so that models can attribute aerosol radiative forcing to different sources. In large-scale models, ...