<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>3</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-2783-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/2783/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/2783/2003/acpd-3-2783-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/2783/2003/acpd-3-2783-2003.pdf</fulltext_pdf>
	<start_page>2783</start_page>
	<end_page>2833</end_page>
	<publication_date>2003-05-23</publication_date>
	<article_title content_type="html">One year boundary layer aerosol size distribution data from five Nordic background stations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Tunved</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>H.-C. Hansson</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. Kulmala</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>P. Aalto</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>Y. Viisanen</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>H. Karlsson</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>A. Kristensson</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>E. Swietlicki</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>M. Dal Maso</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>J. Ström</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>M. Komppula</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Applied Environmental Research, Stockholm University, SE-106 91, Stockholm, Sweden</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics, POB 9, FIN-00014 University of Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">Finnish Meteorological Institute, POB 503, FIN-00101 Helsinki, Finland</affiliation>
		<affiliation numeration="4" content_type="html">Division of Nuclear Physics, POB 118, SE-221 00 Lund University, Sweden</affiliation>
	</affiliations>
	<abstract content_type="html">Size distribution measurements performed at five different stations have been investigated
      during a one-year period between 01 June 2000 and 31 May 2001 with focus on diurnal,
      seasonal and geographical differences of size distribution properties. The stations involved
      cover a large geographical area ranging from the Finnish Lapland (67&amp;deg; N) down to southern
      Sweden (56&amp;deg; N) in the order Värriö, Pallas, Hyytiälä, Aspvreten and
      Vavihill. The shape of the size distribution is typically bimodal during winter with a larger fraction of
      accumulation mode particles compared to the other seasons. Highest Aitken mode
      concentration is found during summer and spring.&lt;br&gt;
      &lt;br&gt;
      The maximum of nucleation events occur during spring months. Nucleation events occur
      during other seasons as well, although not as frequently.&lt;br&gt;
      &lt;br&gt;
      Large differences were found between different categories of stations. Northerly located
      stations such as Pallas and Värriö presented well-separated Aitken and accumulation modes,
      while the two modes often overlap significantly at the two southernmost stations Vavihill and
      Aspvreten.&lt;br&gt;
      &lt;br&gt;
      A method to cluster trajectories was used to analyse the impact of long-range transport on the
      observed aerosol properties. Clusters of trajectories arriving from the continent were clearly
      associated with size distributions shifted towards the accumulation mode. This feature was
      more pronounced the further south the station was located. Marine- or Arctic-type clusters
      were associated with large variability in the nuclei size ranges.&lt;br&gt;
      &lt;br&gt;
      A quasi-lagrangian approach was used to investigate transport related changes in the aerosol
      properties. Typically, an increase in especially Aitken mode concentrations was observed
      when advection from the north occurs, i.e. allowing more continental influence on the aerosol
      when comparing the different measurement sites. When trajectory clusters arrive to the
      stations from SW, a gradual decrease in number concentration is experienced in all modes as
      latitude of measurement site increases.</abstract>
	<references>
	</references>
</article>

