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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-9-5461-2009</article-id>
<title-group>
<article-title>Long term particle size distribution measurements at Mount Waliguan, a high-altitude site in inland China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kivekäs</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sun</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhan</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kerminen</surname>
<given-names>V.-M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hyvärinen</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Komppula</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Viisanen</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hong</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>X.-C.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Deli-Geer</surname>
<given-names></given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lihavainen</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Key Laboratory for Atmospheric Chemistry of CMA, Center for Atmosphere Watch and Services, Chinese Academy of Meteorological Sciences, Beijing 100081, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute P.O. Box 1627, 70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>China GAW Baseline Observatory, Qinghai Meteorological Bureau, Xining 810001, China</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>University of Helsinki, Dept. Physical Sciences, P.O. Box 64, 00014 Univ. of Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>08</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>15</issue>
<fpage>5461</fpage>
<lpage>5474</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/5461/2009/acp-9-5461-2009.html">This article is available from http://www.atmos-chem-phys.net/9/5461/2009/acp-9-5461-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/5461/2009/acp-9-5461-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/5461/2009/acp-9-5461-2009.pdf</self-uri>
<abstract>
<p>Particle number size distributions in size range 12–570 nm were measured
continuously at Mount Waliguan, a remote mountain-top station in inland
China. The station is located at the altitude of 3816 m a.s.l., and some
600–1200 m above the surrounding area. The measurement period lasted from
September 2005 to May 2007. The measurements were verified with independent
CPC measurements at the same site. The average particle concentration in
ambient conditions was 2030 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, which is higher than the values
measured at similar altitude in other regions of the world. On average, the
Aitken mode contributed to roughly half of the particle number concentration.
The concentrations were found to be higher during the summer than during the
winter. The diurnal variation was also investigated and a clear pattern was
found for the nucleation mode during all seasons, so that the nucleation mode
particle concentration increased in the afternoon. The same pattern was
visible in the Aitken mode during the summer, whereas the accumulation mode
did not show any level of diurnal pattern during any season. Excluding the
nucleation mode, the average day-time particle concentrations were not
significantly higher than those measured at night-time, indicating no
systematic pattern of change between planetary boundary layer conditions and
free troposphere conditions. In air masses coming from east, the number
concentration of particles was higher than in other air masses, which
indicates that the air mass might be affected anthropogenic pollution east of
the station. Also other factors, such as active new-particle formation, keep
aerosol number concentrations high in the area.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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