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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>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-1777-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/1777/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/1777/2003/acpd-3-1777-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/1777/2003/acpd-3-1777-2003.pdf</fulltext_pdf>
	<start_page>1777</start_page>
	<end_page>1804</end_page>
	<publication_date>2003-03-28</publication_date>
	<article_title content_type="html">A revised parameterization for gaseous dry deposition in air-quality models</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Zhang</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. R. Brook</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. Vet</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Meteorological Service of Canada, 4905 Dufferin Street, Toronto, Ontario, M3H 5T4, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">A parameterization scheme for calculating gaseous dry deposition velocities in air-quality
      models is revised based on recent study results on non-stomatal uptake of
      O&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;2&lt;/sub&gt; over 5 different vegetation types. Non-stomatal resistance, which includes in-canopy
      aerodynamic resistance, soil resistance and cuticle resistance, for SO&lt;sub&gt;2&lt;/sub&gt;
      and&amp;nbsp; O&lt;sub&gt;3&lt;/sub&gt; is parameterized as a function of friction velocity, relative humidity, leaf area index, and canopy wetness. Non-stomatal resistance for all other species is scaled to those of
      SO&lt;sub&gt;2&lt;/sub&gt; and&amp;nbsp; O&lt;sub&gt;3&lt;/sub&gt; based on their chemical and physical characteristics. Stomatal resistance is calculated using a
      leaf-stomatal-resistance model for all gaseous species of interest. The improvements in the present model compared to its
      earlier version include a newly developed non-stomatal resistance formulation, a realistic
      treatment of cuticle and ground resistance in winter and the handling of seasonally-dependent
      input parameters. Model evaluation shows that the revised parameterization can provide more
      realistic deposition velocities for both&amp;nbsp; O&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;2&lt;/sub&gt;, especially for wet canopies. Example model
      output shows that the parameterization provides reasonable estimates of dry deposition velocities
      for different gaseous species, land types and diurnal and seasonal variations. Maximum
      deposition velocities from model output are close to reported measurement values for different
      land types. The current parameterization can be easily adopted into different air-quality models
      that require inclusion of dry deposition processes.</abstract>
	<references>
	</references>
</article>

