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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>10</volume_number>
		<issue_number>7</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-17753-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/17753/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/17753/2010/acpd-10-17753-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/17753/2010/acpd-10-17753-2010.pdf</fulltext_pdf>
	<start_page>17753</start_page>
	<end_page>17788</end_page>
	<publication_date>2010-07-23</publication_date>
	<article_title content_type="html">Ultrafine particle formation in the inland sea breeze airflow in Southwest Europe</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Fernández-Camacho</name>
			<email>rocio.fernandez@dgeo.uhu.es</email>
		</author>
		<author numeration="2" affiliations="1,3">
			<name>S. Rodríguez</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. de la Rosa</name>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>A. M. Sánchez de la Campa</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>M. Viana</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>A. Alastuey</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>X. Querol</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Huelva, Joint Research Unit to CSIC &quot;Atmospheric Pollution&quot;, Campus El Carmen, 21071 Huelva, Spain</affiliation>
		<affiliation numeration="2" content_type="html">Estación Experimental del Zaidín, CSIC, C/ Profesor Albareda 1, 18008 Granada, Spain</affiliation>
		<affiliation numeration="3" content_type="html">Izaña Atmospheric Research Centre, AEMET Joint Research Unit to CSIC &quot;Studies on Atmospheric Pollution&quot;, La Marina 20, planta 6, Santa Cruz de Tenerife, 38071, Canary Islands, Spain</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Environmental Assessment and Water Research (IDǼA), CSIC, Jordi Girona, 18&amp;ndash;26, 08034, Barcelona, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">Studies on ultrafine particles and air quality have mostly
      focused on vehicle exhaust emissions and on new particle
      formation in &quot;clean&quot; ambient air. Here we present a study
      of the processes contributing to ultrafine particle
      concentrations in an urban coastal area (Huelva, SW Spain)
      where significant anthropogenic emissions of aerosol
      precursors occur. The overall data analysis shows that two
      processes predominantly contribute to the number of particles
      coarser than 2.5 nm: vehicle exhaust emissions and new
      particle formation due to photo-chemical activity. As
      typically occurs in urban areas, vehicle exhaust emissions
      result in high concentrations of black carbon (BC) and
      particles coarser than 2.5 nm (N) during the morning rush
      hours. The highest N concentrations were recorded during the
      11–17 h period, under the sea breeze regime, when
      photochemical activity resulted in high O&lt;sub&gt;3&lt;/sub&gt; levels and
      new particle formation in the aerosol precursors&apos; rich inland
      airflow. In this period, it is estimated that about 80% of
      the number of particles are linked to sulfur dioxide
      emissions. The contributions to N of &quot;carbonaceous
      material and those compounds nucleating/condensing immediately
      after emission&quot; and of the &quot;new particle formation
      processes in air masses rich gaseous precursors (e.g.
     SO&lt;sub&gt;2&lt;/sub&gt;)&quot; were estimated by means of a relatively novel
      method based on simultaneous measurements of BC and
      N. A comparison with two recent studies suggests that the
      daily cycles of  &quot;new particle formation&quot; during the period
      when the inland sea breeze is blowing period seem to be
      a feature of ultrafine particles in coastal areas of
      South-west Europe.</abstract>
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</article>

