2018
DOI: 10.1038/s41598-017-17343-9
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Novel insights on new particle formation derived from a pan-european observing system

Abstract: The formation of new atmospheric particles involves an initial step forming stable clusters less than a nanometre in size (<~1 nm), followed by growth into quasi-stable aerosol particles a few nanometres (~1–10 nm) and larger (>~10 nm). Although at times, the same species can be responsible for both processes, it is thought that more generally each step comprises differing chemical contributors. Here, we present a novel analysis of measurements from a unique multi-station ground-based observing system which re… Show more

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Cited by 52 publications
(45 citation statements)
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“…Cluster analysis has routinely been used to understand SMPS data for over a decade , 2018a, b, 2017aLange et al, 2018;Beddows et al, 2014Beddows et al, , 2009 and is useful in reducing the complexity of multivariate data into a manageable size to understand natural processes in the environment. The cluster analysis procedure is relatively straightforward and consists of three stages: (i) normalization, (ii) cluster choice and (iii) cluster partition.…”
Section: Smps K-mean Clustering Data Analysismentioning
confidence: 99%
“…Cluster analysis has routinely been used to understand SMPS data for over a decade , 2018a, b, 2017aLange et al, 2018;Beddows et al, 2014Beddows et al, , 2009 and is useful in reducing the complexity of multivariate data into a manageable size to understand natural processes in the environment. The cluster analysis procedure is relatively straightforward and consists of three stages: (i) normalization, (ii) cluster choice and (iii) cluster partition.…”
Section: Smps K-mean Clustering Data Analysismentioning
confidence: 99%
“…The Ångström coefficient (å) is computed from multi-wavelength nephelometer measurements according to Equation (6). In this study, we combined the scattering coefficient at 525 nm with the absorption coefficient to get the in situ extinction coefficient (EXT IS ) and aerosol single scattering albedo (ω 0 ) between 520nm and 525 nm according to Equations (7) and (8).…”
Section: Nephelometermentioning
confidence: 99%
“…To understand the effects of aerosol particles on climate and health, measurements of their optical and physical properties, e.g., particle number size distributions, concentrations, aerosol light absorption and scattering in the atmosphere, are needed. Important information on atmospheric aerosol properties have been provided at the European scale, e.g., new particle formation (NPF) [7,8], aerosol-cloud interactions [9,10], and aerosol scattering and absorption [11,12]. These measurements were mostly being performed within the ACTRIS (Aerosols, Clouds, and Trace Gases Research Infrastructure Network) project [13] and all data used in this study are available via the ACTRIS-EBAS data portal (http://ebas.nilu.no/).…”
Section: Introductionmentioning
confidence: 99%
“…S losses takes into account additional losses and was ignored in this study. GR was calculated using the mode-fitting method (Dal Maso et al, 2005).…”
Section: Measurementsmentioning
confidence: 99%