The third Pallas Cloud Experiment: Consistency between the aerosol hygroscopic growth and CCN activity. Jaatinen, A., Romakkaniemi, S., Hao, L., Q., Kortelainen, A., Miettinen, P., Mikkonen, S., Smith, J., N., Virtanen, A., Laaksonen, A., Anttila, T., Hyvärinen, A., P., Smith, J., N., Laaksonen, A., Smith, J., N., & Romakkaniemi, S. Boreal Environment Research, 19:368-382, 2014. Website abstract bibtex Measurements of aerosol chemical and hygroscopic properties and cloud\ncondensation nuclei were carried out as a part of the third Pallas Cloud\nExperiment. In this study, the aerosol hygroscopicity parameter, kappa,\nwas determined using data from instruments operating in the\nsub-saturated and supersaturated water vapour regimes, as well as from\nmeasurements of aerosol chemical composition. During the campaign, kappa\nvaried from similar to 0.01 to similar to 0.37 as derived by Cloud\nCondensation Nuclei counter and Hygroscopic Tandem Differential Mobility\nanalyser data, and from similar to 0.13 to similar to 0.60 as derived\nfrom Aerosol Mass Spectrometer data, the average values being 0.11 and\n0.29, respectively. CCN closure calculations showed that the\nsub-saturated growth factor retrieved CCN concentration is lower than\nthe measured one. Overall, at the Pallas site, aerosol hygroscopicity\nwas size dependent with hygroscopicity increasing with size. Hence, size\ndependent information on composition is needed to predict CCN\nconcentrations relevant to cloud droplet formation.
@article{
title = {The third Pallas Cloud Experiment: Consistency between the aerosol hygroscopic growth and CCN activity},
type = {article},
year = {2014},
keywords = {arctic background site,boreal forest,campaign,condensation nuclei,droplet activation,experiment 2nd pace,finland,mass-spectrometer,microphysics,northern,particles},
pages = {368-382},
volume = {19},
websites = {http://www.borenv.net/BER/pdfs/ber19/ber19B-368.pdf},
id = {60f615b5-26ab-31d1-938c-1472215fb713},
created = {2023-01-31T22:46:08.417Z},
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last_modified = {2023-01-31T22:46:08.417Z},
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hidden = {false},
citation_key = {Jaatinen2014a},
source_type = {Journal Article},
language = {English},
notes = {<b>From Duplicate 1 (<i>The third Pallas Cloud Experiment: Consistency between the aerosol hygroscopic growth and CCN activity</i> - Jaatinen, Antti; Romakkaniemi, Sami; Hao, Li Qing; Kortelainen, Aki; Miettinen, Pasi; Mikkonen, Santtu; Smith, James N.; Virtanen, Annele; Laaksonen, Ari; Anttila, Tatu; Hyvärinen, Antti Pekka; Smith, James N.; Laaksonen, Ari; Smith, James N.; Romakkaniemi, Sami)<br/></b><br/>ISI Document Delivery No.: AQ2XU<br/>Times Cited: 3<br/>Cited Reference Count: 39<br/>Jaatinen, Antti Romakkaniemi, Sami Anttila, Tatu Hyvarinen, Antti-Pekka Hao, Li-Qing Kortelainen, Aki Miettinen, Pasi Mikkonen, Santtu Smith, James N. Virtanen, Annele Laaksonen, Ari<br/>Academy of Finland Center of Excellence program [1118615]; Kone foundation; Saastamoinen Foundation; Finnish Academy; US Department of Energy; US National Science Foundation; UEF Postdoc Research Foundation [930275]<br/>The work has been supported financially by the Academy of Finland Center of Excellence program (project no. 1118615). A.J. was supported by the Kone foundation. S.R. acknowledges the Academy of Finland for the Academy Research Fellow position (decision 267514). J.S. acknowledges support from the Saastamoinen Foundation, the Finnish Academy, and the US Department of Energy. NCAR is supported by the US National Science Foundation. H.L. acknowledges the financial support of the UEF Postdoc Research Foundation (no. 930275).<br/>Finnish environment inst<br/>Helsinki<br/>B<br/>Si},
private_publication = {false},
abstract = {Measurements of aerosol chemical and hygroscopic properties and cloud\ncondensation nuclei were carried out as a part of the third Pallas Cloud\nExperiment. In this study, the aerosol hygroscopicity parameter, kappa,\nwas determined using data from instruments operating in the\nsub-saturated and supersaturated water vapour regimes, as well as from\nmeasurements of aerosol chemical composition. During the campaign, kappa\nvaried from similar to 0.01 to similar to 0.37 as derived by Cloud\nCondensation Nuclei counter and Hygroscopic Tandem Differential Mobility\nanalyser data, and from similar to 0.13 to similar to 0.60 as derived\nfrom Aerosol Mass Spectrometer data, the average values being 0.11 and\n0.29, respectively. CCN closure calculations showed that the\nsub-saturated growth factor retrieved CCN concentration is lower than\nthe measured one. Overall, at the Pallas site, aerosol hygroscopicity\nwas size dependent with hygroscopicity increasing with size. Hence, size\ndependent information on composition is needed to predict CCN\nconcentrations relevant to cloud droplet formation.},
bibtype = {article},
author = {Jaatinen, Antti and Romakkaniemi, Sami and Hao, Li Qing and Kortelainen, Aki and Miettinen, Pasi and Mikkonen, Santtu and Smith, James N. and Virtanen, Annele and Laaksonen, Ari and Anttila, Tatu and Hyvärinen, Antti Pekka and Smith, James N. and Laaksonen, Ari and Smith, James N. and Romakkaniemi, Sami},
journal = {Boreal Environment Research}
}
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Virtanen, Annele Laaksonen, Ari<br/>Academy of Finland Center of Excellence program [1118615]; Kone foundation; Saastamoinen Foundation; Finnish Academy; US Department of Energy; US National Science Foundation; UEF Postdoc Research Foundation [930275]<br/>The work has been supported financially by the Academy of Finland Center of Excellence program (project no. 1118615). A.J. was supported by the Kone foundation. S.R. acknowledges the Academy of Finland for the Academy Research Fellow position (decision 267514). J.S. acknowledges support from the Saastamoinen Foundation, the Finnish Academy, and the US Department of Energy. NCAR is supported by the US National Science Foundation. 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