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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-9-25085-2009</article-id>
<title-group>
<article-title>Optical, physical and chemical characteristics of Australian Desert dust aerosols: results from a field experiment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Radhi</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>Box</surname>
<given-names>M. 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>Box</surname>
<given-names>G. P.</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>Mitchell</surname>
<given-names>R. 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>Cohen</surname>
<given-names>D. D.</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>Stelcer</surname>
<given-names>E.</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>Keywood</surname>
<given-names>M. 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>School of Physics, University of New South Wales, Sydney NSW 2052, Australia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CSIRO Marine and Atmospheric Research, Centre for Australian Weather and Climate Research, a partnership between CSIRO and the Australian Bureau of Meteorology, Australia</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Australian Nuclear Science and Technology Organisation, Menai NSW 2234, Australia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>6</issue>
<fpage>25085</fpage>
<lpage>25125</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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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/25085/2009/acpd-9-25085-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/25085/2009/acpd-9-25085-2009.pdf</self-uri>
<abstract>
<p>Mineral dust is one of the major components of the
world&apos;s aerosol mix, having a number of impacts within the Earth system.
However, the climate forcing impact of mineral dust is currently poorly
constrained, with even its sign uncertain. As Australian deserts are more
reddish than those in the northern hemisphere, it is important to better
understand the physical, chemical and optical properties of this important
aerosol. We have investigated the properties of Australian desert dust at a
site in SW Queensland, which is strongly influenced by both dust and biomass
burning aerosol. Three years of ground-based monitoring of spectral optical
thickness has provided a statistical picture of gross aerosol properties. In
November 2006 we undertook a field campaign which collected 4 sets of
size-resolved aerosol samples for laboratory analysis – both ion beam
analysis and ion chromatography.&lt;br&gt; &lt;br&gt;
The aerosol optical depth data showed a weak seasonal cycle with an annual
mean of 0.06&amp;plusmn;0.03. The Angstrom coefficient showed a stronger cycle,
indicating the influence of the winter-spring burning season in Australia&apos;s
north. Size distribution inversions showed a bimodal character, with the
coarse mode assumed to be mineral dust, and the fine mode a mixture of
biomass burning and marine biogenic material. Ion Beam Analysis was used to
determine the elemental composition of all filter samples, although
elemental ratios were considered the most reliable output. Scatter plots
showed that Fe, Al and Ti were well correlated with Si, and Co reasonably
well correlated, with the Fe/Si ratio higher than the crustal average, as
expected. Scatter plots for Ca, Mn and K against Si showed clear evidence of
a second population, which in some cases could be identified with a
particular sample day or size fraction. Ion Chromatography was used to
quantify water soluble ions for 2 of our sample sets, showing the importance
of marine influences on both fine (biogenic) and coarse (sea salt) modes.</p>
</abstract>
<counts><page-count count="41"/></counts>
</article-meta>
</front>
<body/>
<back>
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