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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-8-19035-2008</article-id>
<title-group>
<article-title>Coastal and open ocean aerosol characteristics: investigating the representativeness of coastal aerosol sampling over the North-East Atlantic Ocean</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rinaldi</surname>
<given-names>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>Facchini</surname>
<given-names>M. 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>Decesari</surname>
<given-names>S.</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>Carbone</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>Finessi</surname>
<given-names>E.</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>Mircea</surname>
<given-names>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>Fuzzi</surname>
<given-names>S.</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>Ceburnis</surname>
<given-names>D.</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>Ehn</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>Kulmala</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>de Leeuw</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>O&apos;Dowd</surname>
<given-names>C. D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Istituto di Scienze dell&apos;Atmosfera e del Clima, Consiglio Nazionale delle Ricerche, Bologna, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Experimental Physics and Environmental Change Institute, National University of Ireland Galway, Galway, Ireland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Division of Atmospheric Sciences and Geophysics, Department of Physics, University of Helsinki, Helsinki, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Research and Development, Climate Change Unit, Atmospheric Modelling and Observations, Finnish Meteorological Institute, Helsinki, Finland</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Unit Environment, Health and Safety, TNO, Utrecht, Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>11</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>6</issue>
<fpage>19035</fpage>
<lpage>19062</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>
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<abstract>
<p>In order to achieve a better understanding of the modifications of the
physical and chemical properties of marine aerosol particles during
transport from offshore to the coast, size distribution and chemical
composition were measured concurrently in clean air masses over the open
North Atlantic Ocean and at an Irish coastal site. Open ocean sampling was
performed on board the oceanographic vessel Celtic Explorer sailing 100–300 km off the Irish west coast, while coastal measurements were performed at
the Mace Head GAW station. The experiment took place between 11 June and 6
July 2006, during the period of phytoplankton bloom.
&lt;br&gt;&lt;br&gt;
The number size distribution and size-resolved chemical composition of
coastal and open ocean samples were very similar, indicating homogeneous
physical and chemical aerosol properties over a wide region in the marine
boundary layer. The results also show that submicron chemical and physical
aerosol properties measured at the coastal Mace Head Atmospheric Research
Station were not unduly influenced by coastal artefacts and are thus
representative of open water properties. Greater differences between the
coastal site and the open ocean were observed for the aerosol supermicron
sea spray components; this could be due to a variety of reasons, ranging
from higher local wind speeds at the coastal site over the comparison
period, to differences in sampling heights and increased local surf-zone
production.
&lt;br&gt;&lt;br&gt;
Evidence of ageing processes was observed: at the costal site the ratio
between non-sea-salt sulphate and methanesulphonic acid was higher, and the
aerosol water soluble organic compounds were more oxidized than in
the open ocean.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
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