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Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna

During a total of 11 months, cloud condensation nuclei (CCN at super-saturation S 0.5%) and condensation nuclei (CN) concentrations were measured in the urban background aerosol of Vienna, Austria. For several months, number size distributions between 13.22 nm and 929 nm were also measured with a sc...

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Autores principales: Burkart, J., Steiner, G., Reischl, G., Hitzenberger, R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Pergamon 2011
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3174422/
https://www.ncbi.nlm.nih.gov/pubmed/21977003
http://dx.doi.org/10.1016/j.atmosenv.2011.07.022
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author Burkart, J.
Steiner, G.
Reischl, G.
Hitzenberger, R.
author_facet Burkart, J.
Steiner, G.
Reischl, G.
Hitzenberger, R.
author_sort Burkart, J.
collection PubMed
description During a total of 11 months, cloud condensation nuclei (CCN at super-saturation S 0.5%) and condensation nuclei (CN) concentrations were measured in the urban background aerosol of Vienna, Austria. For several months, number size distributions between 13.22 nm and 929 nm were also measured with a scanning mobility particle spectrometer (SMPS). Activation ratios (i.e. CCN/CN ratios) were calculated and apparent activation diameters obtained by integrating the SMPS size distributions. Variations in all CCN parameters (concentration, activation ratio, apparent activation diameter) are quite large on timescales of days to weeks. Passages of fronts influenced CCN parameters. Concentrations decreased with the passage of a front. No significant differences were found for fronts from different sectors (for Vienna mainly north to west and south to east). CCN concentrations at 0.5% S ranged from 160 cm(−3) to 3600 cm(−3) with a campaign average of 820 cm(−3). Activation ratios were quite low (0.02–0.47, average: 0.13) and comparable to activation ratios found in other polluted regions (e.g. Cubison et al., 2008). Apparent activation diameters were found to be much larger (campaign average: 169 nm, range: (69–370) nm) than activation diameters for single-salt particles (around 50 nm depending on the salt). Contrary to CN concentrations, which are influenced by source patterns, CCN concentrations did not exhibit distinct diurnal patterns. Activation ratios showed diurnal variations counter-current to the variations of CN concentrations.
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spelling pubmed-31744222011-10-03 Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna Burkart, J. Steiner, G. Reischl, G. Hitzenberger, R. Atmos Environ (1994) Article During a total of 11 months, cloud condensation nuclei (CCN at super-saturation S 0.5%) and condensation nuclei (CN) concentrations were measured in the urban background aerosol of Vienna, Austria. For several months, number size distributions between 13.22 nm and 929 nm were also measured with a scanning mobility particle spectrometer (SMPS). Activation ratios (i.e. CCN/CN ratios) were calculated and apparent activation diameters obtained by integrating the SMPS size distributions. Variations in all CCN parameters (concentration, activation ratio, apparent activation diameter) are quite large on timescales of days to weeks. Passages of fronts influenced CCN parameters. Concentrations decreased with the passage of a front. No significant differences were found for fronts from different sectors (for Vienna mainly north to west and south to east). CCN concentrations at 0.5% S ranged from 160 cm(−3) to 3600 cm(−3) with a campaign average of 820 cm(−3). Activation ratios were quite low (0.02–0.47, average: 0.13) and comparable to activation ratios found in other polluted regions (e.g. Cubison et al., 2008). Apparent activation diameters were found to be much larger (campaign average: 169 nm, range: (69–370) nm) than activation diameters for single-salt particles (around 50 nm depending on the salt). Contrary to CN concentrations, which are influenced by source patterns, CCN concentrations did not exhibit distinct diurnal patterns. Activation ratios showed diurnal variations counter-current to the variations of CN concentrations. Pergamon 2011-10 /pmc/articles/PMC3174422/ /pubmed/21977003 http://dx.doi.org/10.1016/j.atmosenv.2011.07.022 Text en © 2011 Elsevier Ltd. https://creativecommons.org/licenses/by-nc-nd/3.0/ Open Access under CC BY-NC-ND 3.0 (https://creativecommons.org/licenses/by-nc-nd/3.0/) license
spellingShingle Article
Burkart, J.
Steiner, G.
Reischl, G.
Hitzenberger, R.
Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title_full Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title_fullStr Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title_full_unstemmed Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title_short Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
title_sort long-term study of cloud condensation nuclei (ccn) activation of the atmospheric aerosol in vienna
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3174422/
https://www.ncbi.nlm.nih.gov/pubmed/21977003
http://dx.doi.org/10.1016/j.atmosenv.2011.07.022
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