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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-6077-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/6077/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/6077/2007/acpd-7-6077-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/6077/2007/acpd-7-6077-2007.pdf</fulltext_pdf>
	<start_page>6077</start_page>
	<end_page>6112</end_page>
	<publication_date>2007-05-08</publication_date>
	<article_title content_type="html">On the contribution of Aitken mode particles to cloud droplet populations at continental background areas &amp;ndash; a parametric sensitivity study</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Anttila</name>
			<email>tatu.anttila@fmi.fi</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>V.-M. Kerminen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Finnish Meteorological Institute, Research and Development, P.O. Box 503, 00101 Finland</affiliation>
	</affiliations>
	<abstract content_type="html">Aitken mode particles are potentially an important source
of cloud droplets in continental background areas. In order to find out
which physico-chemical properties of Aitken mode particles are most
important regarding their cloud-nucleating ability, we applied a global
sensitivity method to an adiabatic air parcel model simulating the number of
cloud droplets formed on Aitken mode particles, &lt;i&gt;CD&lt;/i&gt;&lt;sub&gt;2&lt;/sub&gt;. The technique
propagates uncertainties in the parameters describing the properties of
Aitken mode to &lt;i&gt;CD&lt;/i&gt;&lt;sub&gt;2&lt;/sub&gt;. The results show that if the Aitken mode particles do
not contain molecules that are able to reduce the particle surface tension
more than 30% and/or decrease the mass accommodation coefficient of
water, &amp;alpha;, below 10&lt;sup&gt;&amp;minus;2&lt;/sup&gt;, the chemical composition and modal properties may
have roughly an equal importance at low updraft velocities characterized by
maximum supersaturations &amp;lt;0.1%. For larger updraft velocities, however,
the particle size distribution is clearly more important than the chemical
composition. In general, &lt;i&gt;CD&lt;/i&gt;&lt;sub&gt;2&lt;/sub&gt; exhibits largest sensitivity to the particle
number concentration, followed by the particle size. Also the shape of the
particle mode, characterized by the geometric standard deviation (GSD), can
be as important as the mode mean size at low updraft velocities. Finally,
the performed sensitivity analysis revealed also that the chemistry may
dominate the total sensitivity of  &lt;i&gt;CD&lt;/i&gt;&lt;sub&gt;2&lt;/sub&gt; to the considered parameters if: 1)
the value of  &amp;alpha; varies at least one order of magnitude more than what is
expected for pure water surfaces (10&lt;sup&gt;&amp;minus;2&lt;/sup&gt;&amp;ndash;1), or 2) the particle surface
tension varies more than roughly 30% under conditions close to reaching
supersaturation.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Anttila, T. and Kerminen, V.-M.: Influence of organic compounds on cloud droplet activation &amp;ndash; a model investigation considering the volatility, water-solubility and surface activity of organic matter, J. Geophys. Res. 107, 4662, doi:10.1029/2001JD001482, 2002. </reference>
		<reference numeration="2" content_type="text"> Asa-Awuku, A. and Nenes, A.: The Effect of Solute Dissolution Kinetics on Cloud Droplet Formation: 1. Extended Köhler theory, J. Geophys. Res.-Atmos., accepted, 2006. </reference>
		<reference numeration="3" content_type="text"> Calbó, J., Pan, W., Webster, M., Prinn, R., and McRae, G.: Parameterization of Urban Sub-Grid Scale Processes in Global Atmospheric Chemistry Models, J. Geophys. Res., 103, 3437&amp;ndash;3452, 1998. </reference>
		<reference numeration="4" content_type="text"> Cantrell, W., Shaw, G., and Benner, R.: Cloud properties inferred from bimodal number distributions, J. Geophys. Res., 104, 27 615&amp;ndash;27 624, 1999. </reference>
		<reference numeration="5" content_type="text"> Chuang, P. Y.: Measurement of the timescale of hygroscopic growth for atmospheric aerosols, J. Geophys. Res. 108, 4282, doi:10.1029/2002JD002757, 2003. </reference>
		<reference numeration="6" content_type="text"> Chuang, P. Y.: Sensitivity of cloud condensation nuclei activation processes to kinetic parameters, J. Geophys. Res., 111, D09201, doi:10.1029/2005JD006529, 2006. </reference>
		<reference numeration="7" content_type="text"> Dinar, E., Taraniuk, I., Graber, E., Katsman, S., Moise, T., Anttila, T., Mentel, T., and Rudich, Y.: Cloud Condensation Nuclei properties of model and atmospheric HULIS, Atmos. Chem. Phys., 6, 2465&amp;ndash;2482, 2006. </reference>
		<reference numeration="8" content_type="text"> Dusek, U., Frank, G. P., Hildebrandt, L., Curtius, J., Schneider, J., Walter, S., Chand, D., Drewnick, F., Hings, S., Jung, D., Borrmann, S., and Andreae, M. O.: Size matters more than chemistry for cloud-nucleating ability of aerosol particles, Science, 312, 1375&amp;ndash;1378, 2006. </reference>
		<reference numeration="9" content_type="text"> Ehn, M., Petäjä, T., Aufmhoff, H., Aalto, P., Hämeri, K., Arnold, F., Laaksonen, A., and Kulmala, M.: Hygroscopic properties of ultrafine aerosol particles in the boreal forest: diurnal variation, solubility and the influence of sulfuric acid, Atmos. Chem. Phys., 7, 211&amp;ndash;222, 2007. </reference>
		<reference numeration="10" content_type="text"> Ervens, B., Feingold, G., and Kreidenweis, S. M.: Influence of water-soluble organic carbon on cloud drop number concentration, J. Geophys. Res., 110, D18211, doi:10.1029/2004JD005634, 2005. </reference>
		<reference numeration="11" content_type="text"> Ervens, B., Cubison, M., Andrews, E., Feingold, G., Ogren, J.A., Jimenez, J.L., DeCarlo, P., and Nenes, A.: Prediction of cloud condensation nucleus number concentration using measurements of aerosol size distributions and composition and light scattering enhancement due to humidity, J. Geophys. Res., 112, D10S32, doi:10.1029/2006JD007426, 2007. </reference>
		<reference numeration="12" content_type="text"> Facchini, M. C., Decesari, S., Mircea, M., Fuzzi, S., and Loglio, G.: Surface tension of atmospheric wet aerosol and cloud/fog droplets in relation to their organic carbon content and chemical composition, Atmos. Environ., 34, 4853&amp;ndash;4857, 2000. </reference>
		<reference numeration="13" content_type="text"> Feingold, G.: Modeling of the first indirect effect: Analysis of measurement requirements, Geophys. Res. Lett., 30, 1997, doi:10.1029/2003GL017967, 1997. </reference>
		<reference numeration="14" content_type="text"> Graber, E. R. and Rudich, Y.: Atmospheric HULIS: How humic-like are they? A comprehensive and critical review, Atmos. Chem. Phys., 6, 729&amp;ndash;753, 2006. </reference>
		<reference numeration="15" content_type="text"> Henning, S., Rosenørn, T., D&apos;Anna, B., Gola, A. A., Svenningsson, B., and Bilde, M.: Cloud droplet activation and surface tension of mixtures of slightly soluble organics and inorganic salt, Atmos. Chem. Phys., 5, 575&amp;ndash;582, 2005. </reference>
		<reference numeration="16" content_type="text"> Hyvärinen, A.-P., Lihavainen, H., Gaman, A., Vairila, L., Ojala, H., Kulmala, M., and Viisanen, Y.: Surface tensions and densities of oxalic, malonic, succinic, maleic, malic, and cis-pinonic acids, J. Chem. Eng. Data, 51, 255, 2006. </reference>
		<reference numeration="17" content_type="text"> Isukapalli, S. S.: Uncertainty analysis of transport-transformation models. PhD Thesis, New Brunswick Rutgers, New Jersey State University. New Brunswick, New Jersey, United States of America, 1999. </reference>
		<reference numeration="18" content_type="text"> Kerminen, V.-M., Lihavainen, H., Komppula, M., Viisanen, Y., and Kulmala, M.: Direct observational evidence linking atmospheric aerosol formation and cloud droplet activation, Geophys. Res. Lett., 32, L14803, doi:10.1029/2005GL023130, 2005. </reference>
		<reference numeration="19" content_type="text"> Kiss, G., Tombacz, E., and Hansson, H.-C.: Surface tension effects of humic-like substances in the aqueous extract of tropospheric fine aerosol, J. Atmos. Chem., 50, 279&amp;ndash;294, doi:10.1007/s10874-005-5079-5, 2005. </reference>
		<reference numeration="20" content_type="text"> Kokkola, H., Sorjamaa, R., Peräniemi, A., Raatikainen, T., and Laaksonen, A.: Cloud formation of particles containing humic-like substances, Geophys. Res. Let., 33, L10816, doi:10.1029/2006GL026107, 2006. </reference>
		<reference numeration="21" content_type="text"> Komppula, M., Lihavainen, H., Kerminen, V.-M., Kulmala, M., and Viisanen, Y.: Measurements of cloud droplet activation of aerosol particles at a clean subarctic background site, J. Geophys. Res., 110, D06204, doi:10.1029/2004JD005200, 2005. </reference>
		<reference numeration="22" content_type="text"> Kulmala M., Vehkamäki H., Petäja T., Dal Maso M., Lauri A., Kerminen V.-M., Birmili W., and McMurry P. H.: Formation and growth rates of ultrafine atmospheric particles: a review of observations, J. Aerosol. Sci. 35, 143&amp;ndash;176, 2004. </reference>
		<reference numeration="23" content_type="text"> Kurten T., Kulmala M., Dal Maso M., Suni T., Reissell A., Vehkamaki H., Hari P., Laaksonen A., Viisanen Y., and Vesala T.: Estimation of different forest-related contributions to the radiative balance using observations in southern Finland. Bor. Env. Res., 8, 275&amp;ndash;285, 2003. </reference>
		<reference numeration="24" content_type="text"> Laaksonen, A., Vesala, T., Kulmala, M., Winkler, P. M., and Wagner, P. E.: Commentary on cloud modelling and the mass accommodation coefficient of water, Atmos. Chem. Phys., 5, 461&amp;ndash;464, 2005. </reference>
		<reference numeration="25" content_type="text"> Lohmann, U. and Feichter, J.: Global indirect aerosol effects: a review, Atmos. Chem. Phys. 5, 715&amp;ndash;737, 2005 </reference>
		<reference numeration="26" content_type="text"> Lucas, D. D. and Prinn, R. G.: Parametric sensitivity and uncertainty analysis of dimethylsulfide oxidation in the clear-sky remote marine boundary layer, Atmos. Chem. Phys., 5, 1505&amp;ndash;1525, 2005. </reference>
		<reference numeration="27" content_type="text"> Mayer, M.,Wang, C.,Webster, M., and Prinn, R. G.: Linking Local Air Pollution to Global Chemistry and Climate, J. Geophys. Res.,105, 22 869&amp;ndash;22 896, 2000. </reference>
		<reference numeration="28" content_type="text"> McFiggans, G., Artaxo, P., Baltensperger, U., Coe, H., Facchini, M. C., Feingold, G., Fuzzi, S., Gysel, M., Laaksonen, A., Lohmann, U., Mentel, T. F., Murphy, D. M., O&apos;Dowd, C. D., Snider, J. R., and Weingartner, E.: The effect of physical and chemical aerosol properties on warm cloud droplet activation, Atmos. Chem. Phys., 6, 2593&amp;ndash;2649, 2006. </reference>
		<reference numeration="29" content_type="text"> Menon, S.: Current uncertainties in assessing aerosol effects on climate, Ann. Rev. Environ. Resour., 29, 1&amp;ndash;30, 2004. </reference>
		<reference numeration="30" content_type="text"> Mircea, M., Facchini, M. C., Decesari, S., Fuzzi, S., and Charlson, R. J.: The influence of the organic aerosol component on CCN supersaturation spectra for different aerosol types, Tellus, Ser. B, 54, 74&amp;ndash;81, 2002. </reference>
		<reference numeration="31" content_type="text"> Nenes, A., Charlson, R. J., Facchini, M. C., Kulmala, M., Laaksonen, A., and Seinfeld, J. H.: Can chemical effects on cloud droplet number rival the first indirect effect?, Geophys. Res. Lett., 29, 1848, doi:10.1029/2002GL015295, 2002. </reference>
		<reference numeration="32" content_type="text"> Rissmann, T. A., Nenes, A., and Seinfeld, J. H.: Chemical amplification (or dampening) of the Twomey effect: Conditions derived from droplet activation theory, J. Atmos. Sci., 61, 919&amp;ndash;930, 2004. </reference>
		<reference numeration="33" content_type="text"> Rissman, T. A., VanReken, T. M., Wang, J., Gasparini, R., Collins, D. R., Jonsson, H. H., Brechtel, F. J., Flagan, R. C., and Seinfeld, J. H.: Characterization of ambient aerosol from measurements of cloud condensation nuclei during the 2003 Atmospheric Radiation Measurement Aerosol Intensive Observational Period at the Southern Great Plains site in Oklahoma, J. Geophys. Res., 111, D05S11, doi:10.1029/2004JD005695, 2006. </reference>
		<reference numeration="34" content_type="text"> Salma, I., Ocskay, R., Varga, I., and Maenhaut, W.: Surface tension of atmospheric humic-like substances in connection with relaxation, dilution, and solution pH, Geophys. Res. 111, D23205, doi:10.1029/2005JD007015, 2006. </reference>
		<reference numeration="35" content_type="text"> Saltelli, A.: Sensitivity analysis: Could better methods be used?, J. Geophys. Res., 104, 3789&amp;ndash;3793, 1999. </reference>
		<reference numeration="36" content_type="text"> Saltelli, A., Tarantola, S., and Chan, K. P.-S.: A quantitative model-independent method for global sensitivity analysis of model output, Technometrics, 41, 39&amp;ndash;56, 1999b. </reference>
		<reference numeration="37" content_type="text"> Saxena, P. and Hildemann, L. M.: Water-soluble organics in atmospheric particles: A critical review of the literature and application of thermodynamics to identify candidate compounds, J. Atmos. Chem., 24, 57&amp;ndash;109, 1996. </reference>
		<reference numeration="38" content_type="text"> Seinfeld, J. H. and Pandis, S. N.: Atmospheric chemistry and physics: From air Pollution to climate change, John Wiley, New York, United States of America, 1998. </reference>
		<reference numeration="39" content_type="text"> Shulman, M. L., Jacobson, M. C., Charlson, R. J., Synovec, R. E., and Young, T. E.: Dissolution behaviour and surface tension effects of organic compounds in nucleating cloud droplets, Geophys. Res. Lett., 23, 277&amp;ndash;280, 1996. </reference>
		<reference numeration="40" content_type="text"> Sorjamaa, R., Svenningsson, B., Raatikainen, T., Henning, S., Bilde, M., and Laaksonen, A.: The role of surfactants in Köhler theory reconsidered. Atmos. Chem. Phys., 4, 2107&amp;ndash;2117, 2004. </reference>
		<reference numeration="41" content_type="text"> Sorjamaa, R. and Laaksonen, A.: The influence of surfactant properties on critical supersaturations of cloud condensation nuclei, J. Aerosol Sci., 37, 1730&amp;ndash;1736, 2006. </reference>
		<reference numeration="42" content_type="text"> Spracklen, D. V., Springle, K. J., Carslaw, K. S., Chipperfield, M. P., and Mann, G. P.: A global off-line model of size-resolved aerosol microphysics: I. Model development and prediction of aerosol processes, Atmos. Chem. Phys., 5, 2227&amp;ndash;2252, 2005. </reference>
		<reference numeration="43" content_type="text"> Spracklen, D. V., Carslaw, K. S., Kulmala, M., Kerminen, V.-M., Mann, G. W., and Sihto, S.-L.: The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales, Atmos. Chem. Phys., 6, 5631&amp;ndash;5648, 2006. </reference>
		<reference numeration="44" content_type="text"> Stier, P., Feichter, J., Kinne, S., Kloster, S., Vignati, E., Wilson, J., Ganzeveld, L., Tegen, I., Werner, M., Balkanski, Y., Schulz, M., Boucher, O., Minikin, A., and Petzold, A.: The aerosol-climate model ECHAM5-HAM, Atmos. Chem. Phys. 5, 1125&amp;ndash;1156, 2005. </reference>
		<reference numeration="45" content_type="text"> Svenningsson, B., Hansson, H. C., Martinsson, B., Wiedensohler, A., Swietlicki, E., Cederfelt, S. I., Wendisch, M., Bower, K. N., Choularton, T. W., and Colvile, R. N.: Cloud droplet nucleation scavenging in relation to the size and hygroscopic behaviour of aerosol particles, Atmos. Environ., 31, 2463&amp;ndash;2475, 1997. </reference>
		<reference numeration="46" content_type="text"> Tatang,M., Pan, W., Prinn, R., and McRae, G.: An efficient method for parametric uncertainty analysis of numerical geophysical models, J. Geophys. Res., 102, 21 925&amp;ndash;21 932, 1997. </reference>
		<reference numeration="47" content_type="text"> Tuckermann, R. and Cammenga, H. K.: The surface tension of aqueous solutions of some atmospheric water-soluble organic compounds, Atmos. Environ., 38, 6135&amp;ndash;6138, 2004. </reference>
		<reference numeration="48" content_type="text"> Tunved, P., Hansson, H.-C., Kulmala, M., Aalto, P., Viisanen, Y., Karlsson, H., Kristensson, A., Swietlicki, E., Dal Maso, M., Ström, J., and Komppula, M.: One year boundary layer aerosol size distribution data from five nordic background stations, Atmos. Chem. Phys., 3, 2183&amp;ndash;2205, 2003. </reference>
		<reference numeration="49" content_type="text"> Vignati, E., Wilson, J., and Stier, P.: M7: An efficient size-resolved aerosol microphysics module for large-scale aerosol transport models, J. Geophys. Res., 109, D22202, doi:10.1029/2003JD004485, 2004. </reference>
	</references>
</article>

