검색결과 : 5건
| No. | Article |
|---|---|
| 1 |
Critical cluster size cannot in practice be determined by slope analysis in atmospherically relevant applications Kupiainen-Maatta O, Olenius T, Korhonen H, Malila J, Dal Maso M, Lehtinen K, Vehkamaki H Journal of Aerosol Science, 77, 127, 2014 |
| 2 |
A large source of low-volatility secondary organic aerosol Ehn M, Thornton JA, Kleist E, Sipila M, Junninen H, Pullinen I, Springer M, Rubach F, Tillmann R, Lee B, Lopez-Hilfiker F, Andres S, Acir IH, Rissanen M, Jokinen T, Schobesberger S, Kangasluoma J, Kontkanen J, Nieminen T, Kurten T, Nielsen LB, Jorgensen S, Kjaergaard HG, Canagaratna M, Dal Maso M, Berndt T, Petaja T, Wahner A, Kerminen VM, Kulmala M, Worsnop DR, Wildt J, Mentel TF Nature, 506(7489), 476, 2014 |
| 3 |
Estimating nucleation rates from apparent particle formation rates and vice versa: Revised formulation of the Kerminen-Kulmala equation Lehtinen KEJ, Dal Maso M, Kulmala M, Kerminen VM Journal of Aerosol Science, 38(9), 988, 2007 |
| 4 |
Formation and growth rates of ultrafine atmospheric particles: a review of observations Kulmala M, Vehkamaki H, Petaja T, Dal Maso M, Lauri A, Kerminen VM, Birmili W, McMurry PH Journal of Aerosol Science, 35(2), 143, 2004 |
| 5 |
Analysis of particle formation bursts observed in Finland Clement CF, Pirjola L, dal Maso M, Makela JM, Kulmala M Journal of Aerosol Science, 32(2), 217, 2001 |