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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>6</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-5513-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/5513/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/5513/2003/acpd-3-5513-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/5513/2003/acpd-3-5513-2003.pdf</fulltext_pdf>
	<start_page>5513</start_page>
	<end_page>5546</end_page>
	<publication_date>2003-11-03</publication_date>
	<article_title content_type="html">Particle size distribution and particle mass measurements at urban, near-city and rural level in the Copenhagen area and Southern Sweden</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M. Ketzel</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. Wåhlin</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Kristensson</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>E. Swietlicki</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>R. Berkowicz</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>O. J. Nielsen</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>F. Palmgren</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Environment, National Environmental Research Institute, Roskilde, Denmark</affiliation>
		<affiliation numeration="2" content_type="html">Division of Nuclear Physics, Physics Department, Lund University, Lund, Sweden</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry, University of Copenhagen, Denmark</affiliation>
	</affiliations>
	<abstract content_type="html">Particle size distribution (size-range
      3&amp;ndash;900 nm) and PM10 was measured simultaneously at an urban background station
      in Copenhagen, a near-city background and a rural location during a period in
      September-November 2002. The study investigates the contribution from urban versus regional sources of particle number and mass concentration.&lt;br&gt;
      &lt;br&gt;
      The total particle number (ToN) and NO&lt;sub&gt;x&lt;/sub&gt; are well correlated at the urban and near-city level and show a distinct diurnal
      variation, indicating the common traffic source. The average ToN at the three stations differs by a factor of 3. The
      observed concentrations are 2500 # cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, 4500 # cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and 7700
      # cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; at rural, near-city and urban level, respectively.&lt;br&gt;
      &lt;br&gt;
      PM10 and total particle volume (ToV) are well correlated between the three different stations and show similar
      concentration levels, in average within 30% relative difference, indicating a common source from long-range transport
      that dominates the concentrations at all locations.&lt;br&gt;
      &lt;br&gt;
      Measures to reduce the local urban emissions of NO&lt;sub&gt;x&lt;/sub&gt; and ToN are likely to affect both the street level and urban
      background concentrations, while for PM10 and ToV only measurable effects at the street level are probable. Taking into
      account the supposed stronger health effects of ultrafine particles reduction measures should address particle
      number emissions.&lt;br&gt;
      &lt;br&gt;
      The traffic source contributes strongest in the 10&amp;ndash;200 nm particle size range. The maximum of the size distribution
      shifts from about 20&amp;ndash;30 nm at kerbside to 50&amp;ndash;60 nm at rural level. We also observe particle formation events in the
      3&amp;ndash;20 nm size range at rural location in the afternoon hours, mainly under conditions with low concentrations of pre-existing
      aerosol particles.&lt;br&gt;
      &lt;br&gt;
      The maximum in the size distribution of the &quot;traffic contribution&quot; seems to be shifted to about
      28 nm in the urban location compared to 22 nm at kerbside. Assuming NO&lt;sub&gt;x&lt;/sub&gt; as an inert tracer on urban scale let us estimate that ToN at urban level is
      reduced by 15&amp;ndash;30% compared to kerbside. Particle removal processes, e.g. deposition and coagulation, which are most
      efficient for smallest particle sizes (&amp;lt;20 nm) and condensational growth are likely mechanisms for the loss of particle
      number and the shift in particle size.</abstract>
	<references>
	</references>
</article>

