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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-3-521-2003</article-id>
<title-group>
<article-title>Spatial variation of aerosol properties over Europe derived from satellite observations and comparison with model calculations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Robles González</surname>
<given-names>C.</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>Schaap</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>de Leeuw</surname>
<given-names>G.</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>Builtjes</surname>
<given-names>P. J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>van Loon</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>TNO, Physics and Electronics Laboratory, PO-BOX 96864, NL-2509 JG The Hague, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>TNO, Institute of Environmental Science, Energy Research and Process Innovation, PO-Box 342, NL-7300 AH, Apeldoorn, The Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Utrecht University, Institute of Marine and Atmospheric Sciences, PO-Box 80005, NL-3508 TA, Utrecht, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>05</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>3</issue>
<fpage>521</fpage>
<lpage>533</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/3/521/2003/acp-3-521-2003.html">This article is available from http://www.atmos-chem-phys.net/3/521/2003/acp-3-521-2003.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/3/521/2003/acp-3-521-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/3/521/2003/acp-3-521-2003.pdf</self-uri>
<abstract>
<p>Aerosol optical depths (AOD) and
      Angström coefficients over Europe were retrieved using data from the ATSR-2 radiometer on board the ESA satellite ERS-2, for August 1997. Taking
      advantage of the nadir and forward view of the ATSR-2, the dual view algorithm was used
      over land to eliminate the influence of the surface reflection. Over sea the AOD was retrieved
      using only the forward observations. Retrieved aerosol optical properties are in good
      agreement with those from ground-based sunphotometers. The AOD and Angström
      coefficients together yield information on the column integrated effective aerosol distribution.&amp;nbsp;
      &lt;p  style=&quot;line-height: 20px;&quot;&gt;Observed regional variations of the AOD and
      Angström coefficient are related to anthropogenic emissions of aerosol precursors such as
      SO&lt;sub&gt;2&lt;/sub&gt; and NO&lt;sub&gt;x&lt;/sub&gt; in the major European industrial and urban areas, and their subsequent transformation into the aerosol phase. The
      influence of anthropogenic aerosols such as ammonium sulphate and ammonium nitrate on
      the total AOD is estimated using a regional chemistry transport model. Sulphate is estimated
      to contribute from 15% in very clean areas to 70% in polluted areas, the contribution of nitrate
      is between 5% and 25% over most of Europe. This paper shows the great importance of
      nitrate in summer over The Netherlands.</p>
</abstract>
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</article-meta>
</front>
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