Bianchi, FedericoTröstl, JasminJunninen, HeikkiFrege, CarlaHenne, StephanHoyle, Christopher R.Molteni, UgoHerrmann, ErikAdamov, AlexeyBukowiecki, NicolasChen, XuemengDuplissy, JonathanGysel, MartinHutterli, ManuelKangasluoma, JuhaKontkanen, JenniKürten, AndreasManninen, Hanna E.Münch, SteffenPeräkylä, OtsoPetäjä, TuukkaRondo, LindaWilliamson, ChristinaWeingartner, ErnestCurtius, JoachimWorsnop, Douglas R.Kulmala, MarkkuDommen, JosefBaltensperger, Urs2024-01-212024-01-2120160036-80751095-920310.1126/science.aad5456https://irf.fhnw.ch/handle/11654/43912https://doi.org/10.26041/fhnw-7822From neutral to new Many of the particles in the troposphere are formed in situ, but what fraction of all tropospheric particles do they constitute and how exactly are they made? Bianchi et al report results from a high-altitude research station. Roughly half of the particles were newly formed by the condensation of highly oxygenated multifunctional compounds. A combination of laboratory results, field measurements, and model calculations revealed that neutral nucleation is more than 10 times faster than ion-induced nucleation, that particle growth rates are size-dependent, and that new particle formation occurs during a limited time window.en500 - Naturwissenschaften01A - Beitrag in wissenschaftlicher Zeitschrift1109-1112