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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-5-515-2005</article-id>
<title-group>
<article-title>To what extent can aerosol water explain the discrepancy between model calculated and gravimetric PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt;?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tsyro</surname>
<given-names>S. G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Norwegian Meteorological Institute, Oslo, Norway</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>02</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>515</fpage>
<lpage>532</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/5/515/2005/acp-5-515-2005.html">This article is available from http://www.atmos-chem-phys.net/5/515/2005/acp-5-515-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/515/2005/acp-5-515-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/515/2005/acp-5-515-2005.pdf</self-uri>
<abstract>
<p>Inter-comparisons of European air quality models show that regional
transport models, including the EMEP (Co-operative Programme for monitoring
and evaluation of the long-range transmission of air pollutants in Europe)
aerosol model, tend to underestimate the observed concentrations of
PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt;. Obviously, an accurate representation of the
individual aerosol constituents is a prerequisite for adequate calculation
of PM concentrations. On the other hand, available measurements on the
chemical characterization of ambient particles reveal that full chemical PM
mass closure is rarely achieved. The fraction unaccounted for by chemical
analysis can comprise as much as 30-40% of gravimetric PM&lt;sub&gt;10&lt;/sub&gt; or
PM&lt;sub&gt;2.5&lt;/sub&gt; mass. The unaccounted PM mass can partly be due to non-C atoms in
organic aerosols and/or due to sampling and measurement artefacts. Moreover,
a part of the unaccounted PM mass is likely to consist of water associated
with particles. Thus, the gravimetrically measured particle mass does not
necessarily represent dry PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; mass. This is thought to
be one of the reasons for models under-prediction of observed PM, if
calculated dry PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations are compared with
measurements. The EMEP aerosol model has been used to study to what extent
particle-bound water can explain the chemically unidentified PM mass in
filter-based particle samples. Water content of PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&lt;sub&gt;10&lt;/sub&gt; has
been estimated with the model for temperature 20&amp;deg;C and relative humidity
50%, which are conditions required for equilibration of dust-loaded
filters according to the Reference method recommended by the European
Committee for Standardization (CEN). Model calculations for Europe show
that, depending on particle composition, particle-bound water constitutes
20-35% of the annual mean PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations, which
is consistent with existing experimental estimates. At two Austrian sites,
in Vienna and Streithofen, where daily measurements of PM&lt;sub&gt;2.5&lt;/sub&gt; mass and
chemical composition are available, calculated PM&lt;sub&gt;2.5&lt;/sub&gt; water content is
found to be about 75-80% of the undetermined PM&lt;sub&gt;2.5&lt;/sub&gt; mass and there is
correlation between them. Furthermore, accounting for aerosol water has
improved the agreement between modelled and measured daily PM&lt;sub&gt;2.5&lt;/sub&gt;
concentrations, whilst model calculated dry PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations appear
to agree quite well with the total identified PM&lt;sub&gt;2.5&lt;/sub&gt; mass. No
information on the composition of PM measured at EMEP sites is presently
available. Given that PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations are measured
at EMEP stations with gravimetric methods they are likely to contain water.
We show that the levels of modelled PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations
with aerosol water included agree with measurements better than dry PM
concentrations. As expected, the spatial correlation has not changed
significantly, whereas the temporal correlation of daily PM&lt;sub&gt;10&lt;/sub&gt; and
PM&lt;sub&gt;2.5&lt;/sub&gt; with monitoring data has slightly improved at most of the EMEP
sites. Our results suggest that aerosol water should be accounted for in
modelled PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; when compared with filter-based
gravimetric measurements.</p>
</abstract>
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