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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-6-2525-2006</article-id>
<title-group>
<article-title>Atmospheric transport and deposition of Indonesian volcanic emissions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pfeffer</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>Langmann</surname>
<given-names>B.</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>Graf</surname>
<given-names>H.-F.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of the Atmosphere in the Earth System, Max-Planck-Institute for Meteorology, Hamburg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Geography, University of Cambridge, Cambridge, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>06</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>9</issue>
<fpage>2525</fpage>
<lpage>2537</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.net/6/2525/2006/acp-6-2525-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/2525/2006/acp-6-2525-2006.pdf</self-uri>
<abstract>
<p>A regional climate model has been used to study the transport and deposition of
sulfur (SO&lt;sub&gt;2&lt;/sub&gt; and SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;) and PbCl&lt;sub&gt;2&lt;/sub&gt; emissions
from Indonesian volcanoes. The sensitivity of the atmospheric loss of these
trace species to meteorological conditions and their solubility was examined.
Two experiments were conducted: 1) volcanic sulfur
released as primarily SO&lt;sub&gt;2&lt;/sub&gt; and subject to transport, deposition, and
oxidation to SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;; and 2) PbCl&lt;sub&gt;2&lt;/sub&gt; released as an infinitely
soluble passive tracer subject to only transport and deposition. The first experiment
was used to calculate SO&lt;sub&gt;2&lt;/sub&gt; loss rates from each active Indonesian volcano
producing an annual mean loss rate for all volcanoes of 1.1&amp;times;10&lt;sup&gt;-5&lt;/sup&gt; s&lt;sup&gt;-1&lt;/sup&gt;,
or an e-folding rate of approximately 1 day. SO&lt;sub&gt;2&lt;/sub&gt; loss rate was found to
vary seasonally, be poorly correlated with wind speed, and uncorrelated with
temperature or relative humidity. The variability of SO&lt;sub&gt;2&lt;/sub&gt; loss rates is found to
be correlated with the variability of wind speeds, suggesting that it is much more
difficult to establish a &quot;typical&apos;&apos; SO&lt;sub&gt;2&lt;/sub&gt; loss rate for volcanoes that are exposed
to changeable winds. Within an average distance of 70 km away from the
active Indonesian volcanoes, 53% of SO&lt;sub&gt;2&lt;/sub&gt; loss is due to conversion to
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;, 42% due to dry deposition, and 5% due to lateral
transport away from the dominant direction of plume travel. The solubility of
volcanic emissions in water is shown to influence their atmospheric transport and
deposition.  High concentrations of PbCl&lt;sub&gt;2&lt;/sub&gt; are predicted to be deposited near to
the volcanoes while volcanic S travels further away until removal from
the atmosphere primarily via the wet deposition of H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;. The
ratio of the concentration of PbCl&lt;sub&gt;2&lt;/sub&gt; to SO&lt;sub&gt;2&lt;/sub&gt; is found to
exponentially decay at increasing distance from the volcanoes. The more rapid
removal of highly soluble species should be considered when observing
SO&lt;sub&gt;2&lt;/sub&gt; in an aged plume and relating this concentration to other
volcanic species. An assumption that the ratio between the concentrations of
highly soluble volcanic compounds and SO&lt;sub&gt;2&lt;/sub&gt; within a plume
is equal to that observed in fumarolic gases is reasonable at small distances from
the volcanic vent, but will result in an underestimation of the emission flux of highly
soluble species.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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