CCN production by new particle formation in the free troposphere

dc.contributor.authorClémence Rose
dc.contributor.authorKarine Sellegri
dc.contributor.authorIsabel Moreno
dc.contributor.authorFernando Velarde
dc.contributor.authorMichel Ramonet
dc.contributor.authorKay Weinhold
dc.contributor.authorRadovan Krejčí
dc.contributor.authorMarcos Andrade
dc.contributor.authorAlfred Wiedensohler
dc.contributor.authorPatrick Ginot
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T13:54:04Z
dc.date.available2026-03-22T13:54:04Z
dc.date.issued2017
dc.descriptionCitaciones: 108
dc.description.abstractAbstract. Global models predict that new particle formation (NPF) is, in some environments, responsible for a substantial fraction of the total atmospheric particle number concentration and subsequently contributes significantly to cloud condensation nuclei (CCN) concentrations. NPF events were frequently observed at the highest atmospheric observatory in the world, on Chacaltaya (5240 m a.s.l.), Bolivia. The present study focuses on the impact of NPF on CCN population. Neutral cluster and Air Ion Spectrometer and mobility particle size spectrometer measurements were simultaneously used to follow the growth of particles from cluster sizes down to ∼ 2 nm up to CCN threshold sizes set to 50, 80 and 100 nm. Using measurements performed between 1 January and 31 December 2012, we found that 61 % of the 94 analysed events showed a clear particle growth and significant enhancement of the CCN-relevant particle number concentration. We evaluated the contribution of NPF, relative to the transport and growth of pre-existing particles, to CCN size. The averaged production of 50 nm particles during those events was 5072, and 1481 cm−3 for 100 nm particles, with a larger contribution of NPF compared to transport, especially during the wet season. The data set was further segregated into boundary layer (BL) and free troposphere (FT) conditions at the site. The NPF frequency of occurrence was higher in the BL (48 %) compared to the FT (39 %). Particle condensational growth was more frequently observed for events initiated in the FT, but on average faster for those initiated in the BL, when the amount of condensable species was most probably larger. As a result, the potential to form new CCN was higher for events initiated in the BL (67 % against 53 % in the FT). In contrast, higher CCN number concentration increases were found when the NPF process initially occurred in the FT, under less polluted conditions. This work highlights the competition between particle growth and the removal of freshly nucleated particles by coagulation processes. The results support model predictions which suggest that NPF is an effective source of CCN in some environments, and thus may influence regional climate through cloud-related radiative processes.
dc.identifier.doi10.5194/acp-17-1529-2017
dc.identifier.urihttps://doi.org/10.5194/acp-17-1529-2017
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/43380
dc.language.isoen
dc.publisherCopernicus Publications
dc.relation.ispartofAtmospheric chemistry and physics
dc.sourceCentre National de la Recherche Scientifique
dc.subjectCloud condensation nuclei
dc.subjectTroposphere
dc.subjectParticle (ecology)
dc.subjectParticle number
dc.subjectAerosol
dc.subjectCluster (spacecraft)
dc.subjectCondensation
dc.subjectPopulation
dc.subjectAtmospheric sciences
dc.subjectParticle size
dc.titleCCN production by new particle formation in the free troposphere
dc.typearticle

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