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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-11-5785-2011</article-id>
<title-group>
<article-title>Quantifying the magnitude of a missing hydroxyl radical source in a tropical rainforest</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Whalley</surname>
<given-names>L. K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Edwards</surname>
<given-names>P. 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>Furneaux</surname>
<given-names>K. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Goddard</surname>
<given-names>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>Ingham</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Evans</surname>
<given-names>M. J.</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>Stone</surname>
<given-names>D.</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>Hopkins</surname>
<given-names>J. R.</given-names>
</name>
<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>Jones</surname>
<given-names>C. E.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Karunaharan</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lee</surname>
<given-names>J. D.</given-names>
</name>
<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>Lewis</surname>
<given-names>A. C.</given-names>
</name>
<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>Monks</surname>
<given-names>P. S.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Moller</surname>
<given-names>S. J.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heard</surname>
<given-names>D. E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Chemistry, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Centre for Atmospheric Science, University of Leeds, Leeds, LS2 9JT, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Earth and Environment, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Chemistry Department, University of York, Heslington, YO10 5DD, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>National Centre for Atmospheric Science, University of York, Heslington, YO10 5DD, UK</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Chemistry, University of Leicester, University Road, Leicester LE1 7RH, UK</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>deceased</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>02</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>2</issue>
<fpage>5785</fpage>
<lpage>5809</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/11/5785/2011/acpd-11-5785-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/5785/2011/acpd-11-5785-2011.pdf</self-uri>
<abstract>
<p>The lifetime of methane is controlled to a very large extent by the abundance
of the OH radical. The tropics are a key region for methane removal, with
oxidation in the lower tropical troposphere dominating the global methane
removal budget (Bloss et al., 2005). In tropical forested environments where
biogenic VOC emissions are high and NO&lt;sub&gt;x&lt;/sub&gt; concentrations are low, OH
concentrations are assumed to be low due to rapid reactions with sink species
such as isoprene. New, simultaneous measurements of OH concentrations and OH
reactivity, &lt;i&gt;k&lt;/i&gt;&apos;&lt;sub&gt;OH&lt;/sub&gt;, in a Borneo rainforest are reported
and show much higher OH than predicted, with mean peak concentrations of
~2.5&amp;times;10&lt;sup&gt;6&lt;/sup&gt; molecule cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (10 min average) observed around
solar noon. Whilst &lt;i&gt;j&lt;/i&gt;(O&lt;sup&gt;1&lt;/sup&gt;D) and humidity were high, low O&lt;sub&gt;3&lt;/sub&gt;
concentrations limited the OH production from O&lt;sub&gt;3&lt;/sub&gt; photolysis. Measured OH
reactivity was very high, peaking at a diurnal average of
29.1 Â± 8.5 s&lt;sup&gt;âˆ’1&lt;/sup&gt;, corresponding to an OH lifetime of only 34 ms. To
maintain the observed OH concentration given the measured OH reactivity
requires a rate of OH production approximately 10 times greater than
calculated using all measured OH sources. A test of our current understanding
of the chemistry within a tropical rainforest was made using a detailed
zero-dimensional model to compare with measurements. The model over-predicted
the observed HO&lt;sub&gt;2&lt;/sub&gt; concentrations and significantly under-predicted OH
concentrations. Inclusion of an additional OH source formed as a recycled
product of OH initiated isoprene oxidation improved the modelled OH agreement
but only served to worsen the HO&lt;sub&gt;2&lt;/sub&gt; model/measurement agreement. To
replicate levels of both OH and HO&lt;sub&gt;2&lt;/sub&gt;, a process that recycles HO&lt;sub&gt;2&lt;/sub&gt; to
OH is required; equivalent to the OH recycling effect of 0.74 ppbv of NO.
This recycling step increases OH concentrations by 88% at noon and has
wide implications, leading to much higher predicted OH over tropical forests,
with a concomitant reduction in the CH&lt;sub&gt;4&lt;/sub&gt; lifetime and increase in the
rate of VOC degradation.</p>
</abstract>
<counts><page-count count="25"/></counts>
</article-meta>
</front>
<body/>
<back>
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