Abstract

Abstract. 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.

Highlights

  • Atmospheric aerosol particles are known to affect air quality, health (Seaton et al, 1995) and climate

  • Using potential cloud condensation nuclei (CCN) activation diameters 50, 80 and 100 nm, we found that 61 % of the type I new particle formation (NPF) events included in the analysis lead to CCN number concentration increase, with higher probabilities during the wet season (79 %) explained by faster particle growth

  • When comparing the CCN production from NPF with the number concentration of pre-existing CCN transported to the site, we found that NPF was on average responsible for the largest contribution to the CCN concentration, especially during the wet season

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Summary

Introduction

Atmospheric aerosol particles are known to affect air quality, health (Seaton et al, 1995) and climate. Beside their direct interaction with the solar and telluric radiations, aerosol. C. Rose et al.: CCN production by new particle formation in the free troposphere particles act as condensation nuclei for cloud droplets. Rose et al.: CCN production by new particle formation in the free troposphere particles act as condensation nuclei for cloud droplets Cloud effects such as cloud albedo (Twomey, 1977) and lifetime (Albrecht, 1989) constitute the largest uncertainty in the estimation of the radiative forcing of the Earth’s atmosphere (IPCC, 2013). Besides the processing of primary particles, other CCN sources were identified, such as regional new particle formation (NPF) events (Kerminen et al, 2012)

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