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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>9</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-9551-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/9551/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/9551/2009/acpd-9-9551-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/9551/2009/acpd-9-9551-2009.pdf</fulltext_pdf>
	<start_page>9551</start_page>
	<end_page>9595</end_page>
	<publication_date>2009-04-16</publication_date>
	<article_title content_type="html">A comparison of water uptake by aerosols using two thermodynamic models</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Xu</name>
			<email>lixum@umich.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. E. Penner</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>S. Metzger</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>J. Lelieveld</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric, Oceanic and Space Science, University of Michigan,  Ann Arbor, Michigan, USA</affiliation>
		<affiliation numeration="2" content_type="html">Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A comprehensive comparison between two aerosol thermodynamic
      equilibrium models used in chemistry-climate simulations, EQUISOLV II
      and EQSAM3, is conducted for various relative humidities and chemical
      compositions. Our results show that the concentration of total
      particulate matter as well as the associated aerosol liquid water
      content predicted by these two models is comparable for all
      conditions, which is important for radiative forcing estimates. The
      normalized absolute difference in the concentration of total
      particulate matter is 6% on average for all 200 conditions studied,
      leading to a regression coefficient of about 0.8 for the water
      associated with the aerosol between these two models. Relatively large
      discrepancies occur, however, at high ammonium, low nitrate/sodium
      concentrations at low and medium relative humidities (RH&amp;lt;60–70%), which is analyzed and discussed in detail. In addition,
      the prediction of the partitioning of ammonium and nitrate is
      investigated under realistic atmospheric conditions. The data
      collected during the Mediterranean Intensive Oxidant Study (MINOS)
      campaign are simulated using both models. The results show that both
      models can reproduce the concentration of total particulate matter for
      90% of the time within a factor of 2, while the predicted
      concentration of aerosol water by these two models is significantly
      correlated. The largest difference exists near RH&apos;s of 70–80% which
      is the RH range for the transition of mixed ammonium salts from the
      solid to the liquid phase.</abstract>
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</article>

