<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>9</volume_number>
		<issue_number>12</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-4131-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/4131/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/4131/2009/acp-9-4131-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/4131/2009/acp-9-4131-2009.pdf</fulltext_pdf>
	<start_page>4131</start_page>
	<end_page>4144</end_page>
	<publication_date>2009-06-22</publication_date>
	<article_title content_type="html">The relationship between aerosol and cloud drop number concentrations in a global aerosol microphysics model</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>K. J. Pringle</name>
			<email>pringle@mpch-mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>K. S. Carslaw</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>D. V. Spracklen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>G. M. Mann</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. P. Chipperfield</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK</affiliation>
		<affiliation numeration="2" content_type="html">now at: Max-Planck-Institute for Chemistry, Mainz, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Empirical relationships that link cloud droplet number (CDN) to aerosol number
or mass are commonly used to calculate global fields of CDN for climate forcing
assessments.  In this work we use a sectional global model of sulfate and sea-salt
aerosol coupled to a mechanistic aerosol activation scheme  to explore the
limitations of this approach.  We find that a given aerosol number concentration
produces a wide range of CDN concentrations due to variations in the shape of the
aerosol size distribution. On a global scale, the dependence of CDN on the size
distribution results in regional biases in predicted CDN (for a given aerosol
number).  Empirical relationships between aerosol number and CDN are often
derived from regional data but applied to the entire globe.  In an analogous
process, we derive regional &quot;correlation-relations&quot; between aerosol number
and CDN and apply these regional relations to calculations of CDN on the global
scale.  The global mean percentage error in CDN caused by using regionally
derived CDN-aerosol relations is 20 to 26%, which is about half the global
mean percentage change in CDN caused by doubling the updraft velocity. However,
the error is as much as 25–75% in the Southern Ocean, the Arctic and regions
of persistent stratocumulus when an aerosol-CDN correlation relation from the
North Atlantic is used. These regions produce much higher CDN concentrations
(for a given aerosol number) than predicted by the globally uniform empirical
relations. CDN-aerosol number relations from different regions also show very
different sensitivity to changing aerosol. The magnitude of the rate of change
of CDN with particle number, a measure of the aerosol efficacy, varies by a
factor 4. CDN in cloud processed regions of persistent stratocumulus is
particularly sensitive to changing aerosol number. It is therefore likely
that the indirect effect will be underestimated in these important regions.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Abdul-Razzak, H. and Ghan, S J.: A parameterization of aerosol activation, 2, Multiple aerosol types, J. Geophys. Res.-Atmos., 105, 6837–6844, \doi10.1029/1999JD901161, 2000. </reference>
		<reference numeration="2" content_type="text"> Abdul-Razzak, H. and Ghan, S J.: A parameterization of aerosol activation 3. Sectional representation, J. Geophys. Res.-Atmos., 107, 4026, \doi10.1029/2001JD000483, 2002. </reference>
		<reference numeration="3" content_type="text"> Abdul-Razzak, H., Ghan, S J., and Rivera-Carpio, C.: A parameterization of aerosol activation 1. Single aerosol type, J. Geophys. Res.-Atmos., 103, 6123–6132, \doi10.1029/97JD03735, 1998. </reference>
		<reference numeration="4" content_type="text"> Adams, P. and Seinfeld, J.: Disproportionate impact of particulate emissions on global cloud condensation nuclei concentrations, Geophys. Res. Lett., 30, 43–46, 2003. </reference>
		<reference numeration="5" content_type="text"> Andreae, M O. and Rosenfeld, D.: Aerosol-cloud-precipitation interactions. Part 1. The nature and sources of cloud-active aerosols, Earth. Sci. Rev., 89, 13–41, \doi10.1016/j.earscirev.2008.03.001, 2008. </reference>
		<reference numeration="6" content_type="text"> Bauer, E., Petoukhov, V., Ganopolski, A., and Eliseev, A.: Climatic response to anthropogenic sulphate aerosols versus well-mixed greenhouse gases from 1850 to 2000 AD in CLIMBER-2, J. Geophys. Res.-Atmos., 60, 82–97, 2008. </reference>
		<reference numeration="7" content_type="text"> Benkovitz, C.: Global gridded inventories of anthropogenic emissions of sulfur and nitrogen, J. Geophys. Res.-Atmos., 101, 29239–29253, 1996. </reference>
		<reference numeration="8" content_type="text"> Bennartz, R.: Global assessment of marine boundary layer cloud droplet number concentration from satellite, J. Geophys. Res.-Atmos., 112, D02201, \doi10.1029/2006JD007547, 2007. </reference>
		<reference numeration="9" content_type="text"> Boucher, O. and Lohmann, U.: The sulfate-CCN-cloud. albedo effect, A sensitivity study with two general circulation models, Tellus Ser. B., 47, 281–300, 1995. </reference>
		<reference numeration="10" content_type="text"> Chen, Y. and Penner, J E.: Uncertainty analysis for estimates of the first indirect aerosol effect, Atmos. Chem. Phys., 5, 2935–2948, 2005. </reference>
		<reference numeration="11" content_type="text"> Chipperfield, M.: New Version of the TOMCAT/SLIMCAT Off-Line Chemical Transport Model: Intercomparison of Stratospheric Tracer Experiments, Q. J. Roy. Meteor. Soc., 132, 1179–1203, \doi10.1256/qj.05.51, 2006. </reference>
		<reference numeration="12" content_type="text"> Chuang, C., Penner, J., Prospero, J., Grant, K., Rau, G., and Kawamoto, K.: Cloud susceptibility and the first aerosol indirect forcing: Sensitivity to black carbon and aerosol concentrations, J. Geophys. Res.-Atmos., 107(D21), \doi10.1029/2000JD000215, 2002. </reference>
		<reference numeration="13" 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, 1375–1378, \doi10.1126/science.1125261, 2006. </reference>
		<reference numeration="14" content_type="text"> Forster, P., Ramaswamy, V., Artaxo, P., Berntsen, T., Betts, R., Fahey, D., Haywood, J., Lean, J., Lowe, D., Myhre, G., Nganga, J., Prinn, R., Raga, G., Schulz, M., and Van~Dorland, R.: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, 2007. </reference>
		<reference numeration="15" content_type="text"> Fountoukis, C. and Nenes, A.: Continued Development of a Cloud Droplet Formation Parameterization for Global Climate Models, J. Geophys. Res.-Atmos., 110, D11212, \doi10.1029/2004JD005591, 2005. </reference>
		<reference numeration="16" content_type="text"> Fountoukis, C., Nenes, A., Meskhidze, N., Bahreini, R., Conant, W C., Jonsson, H Murphy, S., Sorooshian, A., Varutbangkul, V., Brechtel, F., Flagan, R C., and Seinfeld, J H.: Aerosol cloud drop concentration closure for clouds sampled during the International Consortium for Atmospheric Research on Transport and Transformation 2004 campaign, J. Geophys. Res.-Atmos., 112, D10S30, \doi10.1029/2006JD007272, 2007. </reference>
		<reference numeration="17" content_type="text"> Ghan, S., Easter, R., Hudson, J., and Breon, F.-M.: Evaluation of aerosol indirect radiative forcing in MIRAGE, J. Geophys. Res.-Atmos., 106, 5317–5334, 2001. </reference>
		<reference numeration="18" content_type="text"> Gultepe, I. and Isaac, G A.: Scale effects on averaging of cloud droplet and aerosol number concentrations: observations and models, J. Climate, 12, 1268–1279, 1999. </reference>
		<reference numeration="19" content_type="text"> Hallberg, A., Noone, K J., and Ogren, J A.: Aerosol particles and clouds: which particles form cloud droplets?, Tellus. B, 50, 59–75, 1998. </reference>
		<reference numeration="20" content_type="text"> Jones, A., Roberts, D., and Slingo, A.: A climate model study of indirect radiative forcing by anthropogenic sulfate aerosols, Nature, 370, 450–453, 1994. </reference>
		<reference numeration="21" content_type="text"> Jones, A., Roberts, D., Woodage, M., and Johnson, C.: Indirect sulphate aerosol forcing in a climate model with an interactive sulphur cycle, J. Geophys. Res.-Atmos., 106, 20293–20310, 2001. </reference>
		<reference numeration="22" content_type="text"> Kiehl, J., Schneider, T L., Rasch, P J., Barth, M C., and Wong, J.: Radiative forcing due to sulfate aerosols from simulations with the National Center for Atmospheric Research Community Climate Model, version 3, J. Geophys. Res.-Atmos., 105, 1441–1458, 2000. </reference>
		<reference numeration="23" content_type="text"> Kirkevag, A., Iversen, T., Kristjansson, J E., Seland, Ø., and Debernard, J B.: On the additivity of climate response to anthropogenic aerosols and CO2, and the enhancement of future global warming by carbonaceous aerosols, Tellus A, 60A, 513–527, 2008. </reference>
		<reference numeration="24" 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.-Atmos., 110, D06204, \doihttp://dx.doi.org/10.1029/2004JD005200, 2005. </reference>
		<reference numeration="25" content_type="text"> Korhonen, H., Carslaw, K S., Spracklen, D V., Mann, G., and Woodhouse, M.: Influence of oceanic DMS emissions on CCN concentrations and seasonality over the remote southern hemisphere oceans: A global model study, J. Geophys. Res.-Atmos., 113(D12), \doi10.1029/2007JD009718, 2008. </reference>
		<reference numeration="26" content_type="text"> Kristjansson, J E.: Studies of the aerosol indirect effect from sulfate and black carbon aerosols, J. Geophys. Res.-Atmos., 107(D15), \doi10.1029/2001JD000887, 2002. </reference>
		<reference numeration="27" content_type="text"> Kristjansson, J E., Iversen, T., Kirkev&amp;aring;g, A., Seland, Ø., and Debernard, J.: Response of the climate system to aerosol direct and indirect forcing: Role of cloud feedbacks, J. Geophys. Res.-Atmos., 110, D24206, \doi10.1029/2005JD006299, 2005. </reference>
		<reference numeration="28" content_type="text"> Kulmala, M., Laaksonen, A., and Pirjola, L.: Parameterization for sulfuric acid/water nucleation rates, J. Geophys. Res.-Atmos., 103, 8301–8307, 1998. </reference>
		<reference numeration="29" content_type="text"> Lohmann, U. and Feichter, J.: Global indirect aerosol effects: a review, Atmos. Chem. Phys., 5, 715–737, 2005. </reference>
		<reference numeration="30" content_type="text"> Lohmann, U., Feichter, J., Chuang, C C., and Penner, J E.: Prediction of the number of cloud droplets in the ECHAM GCM, J. Geophys. Res.-Atmos., 104, 9169–9198, 1999. </reference>
		<reference numeration="31" content_type="text"> Lohmann, U., Feichter, J., Penner, J., and Leaitch, R.: Indirect effect of sulfate and carbonaceous aerosols: A mechanistic treatment, J. Geophys. Res.-Atmos., 105, 12193–12206, \doi10.1029/1999JD901199, 2000. </reference>
		<reference numeration="32" content_type="text"> Lowenthal, D H., Borys, R D., Choularton, T W., Bower, K N., Flynn, M J., and Gallagher, M W.: Parameterization of the cloud droplet-sulfate relationship, Atmos. Environ., 38, 287–292, 2004. </reference>
		<reference numeration="33" content_type="text"> Ma, X., von Salzen, K., and Li, J.: Modelling sea salt aerosol and its direct and indirect effects on climate, Atmos. Chem. Phys., 8, 1311–1327, 2008. </reference>
		<reference numeration="34" content_type="text"> Martin, G., Johnson, D., and Spice, A.: The measurement and parameterization of effective radius of droplets in warm stratiform clouds, J. Atmos. Sci., 51, 1823–1842, 1994. </reference>
		<reference numeration="35" content_type="text"> McComiskey, A. and Feingold, G.: Quantifying error in the radiative forcing of the first aerosol indirect effect, Geophys. Res. Lett., 35, L02810, \doi10.1029/2007GL032667, 2008. </reference>
		<reference numeration="36" 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, 2593–2649, 2006. </reference>
		<reference numeration="37" content_type="text"> Menon, S. and Rotstayn, L.: The radiative influence of aerosol effects on liquid-phase cumulus and stratiform clouds based on sensitivity studies with two climate models, Climate Dynam., 27(4), \doi10.1007/s00382-006-0139-3, 2007. </reference>
		<reference numeration="38" content_type="text"> Menon, S., Del~Genio, A D., Dorothy, K., and Tselioudis, G.: GCM simulations of the aerosol indirect effect: Sensitivity to cloud parameterization and aerosol burden, J. Atmos. Sci., 59, 692–713, 2002. </reference>
		<reference numeration="39" content_type="text"> Menon, S., Brenguier, J.-L., Boucher, O., Davison, P., Del~Genio, A D., Feichter, J., Ghan, S., Guibert, S., Liu, X., Lohmann, U., Pawlowska, H., Penner, J E., Quaas, J., Roberts, D L., Schuller, L., and Snider, J.: Evaluating aerosol/cloud/radiation process parameterizations with single-column models and Second Aerosol Characterisation Experiment (ACE-2) cloudy column observations, J. Geophys. Res., 108(D24), \doi10.1029/2003JD003902, 2003. </reference>
		<reference numeration="40" content_type="text"> Meskhidze, N., Nenes, A., Conant, W C., and Seinfeld, J.: Evaluation of a new Cloud Droplet Activation Parameterization with In Situ Data from CRYSTAL-FACE and CSTRIPE, J. Geophys. Res.-Atmos., 110, D16202, \doi10.1029/2004JD005703, 2005. </reference>
		<reference numeration="41" content_type="text"> Meskhidze, N., Sotiropoulou, R. E P., Nenes, A., Kouatchou, J., Das, B., and Rodriguez, J M.: Aerosol-cloud interactions in the NASA GMI: model development and indirect forcing assessments, Atmos. Chem. Phys. Discuss., 7, 14295–14330, 2007. </reference>
		<reference numeration="42" content_type="text"> Ming, Y., Ramaswamy, V., Ginoux, P A., Horowitz, L W., and Russell, L M.: Geophysical Fluid Dynamics Laboratory general circulation model investigation of the indirect radiative effects of anthropogenic sulfate aerosol, J. Geophys. Res.-Atmos., 110, D22206, \doi10.1029/2005JD006161, 2005. </reference>
		<reference numeration="43" content_type="text"> Ming, Y., Ramaswamy, V., Donner, L J., and Phillips, V. T J.: A new parameterization of cloud droplet activation applicable to general circulation models, J. Atmos. Sci., 63, \doi10.1175/JAS3686.11348-1356, 2006. </reference>
		<reference numeration="44" content_type="text"> Nenes, A. and Seinfeld, J H.: Parameterization of cloud droplet formation in global climate models, J. Geophys. Res.-Atmos., 108(4415), \doi10.1029/2002JD002911, 2003. </reference>
		<reference numeration="45" content_type="text"> Penner, J E., Quass, J., Storelvmo, T., Takemura, T Boucher, O., Guo, H., Kirkevag, A., Kristjansson, J E., and Seland, O.: Model intercomparision of indirect aerosol effects, Atmos. Chem. Phys., 6, 3391–3405, 2006. </reference>
		<reference numeration="46" content_type="text"> Quaas, J., Boucher, O., and Lohmann, U.: Constraining the total aerosol indirect effect in the LMDZ and ECHAM4 GCMs using MODIS satellite data, Atmos. Chem. Phys., 6, 947–955, 2006. </reference>
		<reference numeration="47" content_type="text"> Ramanathan, V., Crutzen, P., Kiehl, J., and Rosenfeld, D.: Atmosphere - Aerosols, climate, and the hydrological cycle, Science, 294, 2119–2124, 2001. </reference>
		<reference numeration="48" content_type="text"> Rotstayn, L D., Cai, W., Dix, M R., Farquhar, G D., Feng, Y., Ginoux, P., Herzog, M., Ito, A., Penner, J., Roderick, M L., and Wang, M.: Have Australian rainfall and cloudiness increased due to the remote effects of Asian anthropogenic aerosols?, J. Geophys. Res.-Atmos., 112, D09202, \doi10.1029/2006JD007712, 2007. </reference>
		<reference numeration="49" content_type="text"> Spracklen, D., Pringle, K., Carslaw, K., Chipperfield, M., and Mann, G.: A global off-line model of size resolved aerosol processes; I. Model development and prediction of aerosol properties, Atmos. Chem. Phys., 5, 2227–2252, 2005a. </reference>
		<reference numeration="50" content_type="text"> Spracklen, D., Pringle, K., Carslaw, K., Chipperfield, M., and Mann, G.: A global off-line model of size resolved aerosol processes; II. Importance of uncertainties in microphysical processes, Atmos. Chem. Phys., 5, 3233–3250, 2005b.  </reference>
		<reference numeration="51" 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, 5631–5648, 2006. </reference>
		<reference numeration="52" content_type="text"> Spracklen, D V., Pringle, K J., Carslaw, K S., Mann, G W., Manktelow, P., and Heintzenberg, J.: Evaluation of a global aerosol microphysics model against size-resolved particle statistics in the marine atmosphere, Atmos. Chem. Phys., 7, 2073–2090, 2007. </reference>
		<reference numeration="53" content_type="text"> Stockwell, D. and Chipperfield, M.: A tropospheric chemical -transport model : Development and validation of the model transport schemes, Q. J. Roy. Meteorol. Soc., 125, 1747–1783, 1999. </reference>
		<reference numeration="54" content_type="text"> Takemura, T., Nozawa, T., Emori, S., Nakajima, T Y., and Nakajima, T.: Global three-dimensional simulation of aerosol optical thickness distribution of various origins, J. Geophys. Res.-Atmos., 110, 17853–17874, \doi10.1029/2004JD005029, 2005. </reference>
		<reference numeration="55" content_type="text"> Verma, S., Boucher, O., Upadhyaya, H., and Sharma, O.: Sulfate aerosols forcing: An estimate using a three-dimensional interactive chemistry scheme, Atmos. Environ., 40, 7953–7962, 2006. </reference>
		<reference numeration="56" content_type="text"> Zhang, Y., Easter, R C., Ghan, S J., and Abdul-Razzak, H.: Impact of aerosol size representation on modeling aerosol-cloud interactions, J. Geophys. Res.-Atmos., 107, 4558, \doi10.1029/2001JD001549, 2002. </reference>
	</references>
</article>

