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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-10-5999-2010</article-id>
<title-group>
<article-title>Analysis of accurate &lt;sup&gt;13&lt;/sup&gt;C and &lt;sup&gt;18&lt;/sup&gt;O isotope measurements of CO&lt;sub&gt;2&lt;/sub&gt; in CARIBIC aircraft air samples from the tropical troposphere, and the upper troposphere/lowermost stratosphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Assonov</surname>
<given-names>S. S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<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>Brenninkmeijer</surname>
<given-names>C. A. 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>Schuck</surname>
<given-names>T. J.</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>Taylor</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>European Commission, Joint Research Centre, Institute for Reference Materials and Measurements, Geel, Belgium</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Max Planck Institute for Chemistry, Atmospheric Chemistry Division, Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>presently at: Institute for Geology and Mineralogy, University of Köln, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>03</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>3</issue>
<fpage>5999</fpage>
<lpage>6057</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>The project CARIBIC (&lt;a href=&quot;http://caribic-atmospheric.com&quot;target=&quot;_blank&quot;&gt;http://caribic-atmospheric.com&lt;/a&gt;) aims to study
atmospheric chemistry and transport by regularly measuring many compounds in
the free troposphere (FT) and the upper troposphere/lowermost stratosphere
(UT/LMS) by using passenger aircraft. Here CO&lt;sub&gt;2&lt;/sub&gt; concentrations and
highly accurate isotope results are presented in detail together with
supporting trace gas data. 509 CARIBIC-2 samples (highest precision and
accuracy &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C(CO&lt;sub&gt;2&lt;/sub&gt;) and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O(CO&lt;sub&gt;2&lt;/sub&gt;) data)
from June 2007 until March 2009, together with CARIBIC-1 samples (flights
between November 1999 and April 2002, 350 samples in total, 270 for NH,
mostly &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C(CO&lt;sub&gt;2&lt;/sub&gt;) data) give a fairly extensive, unique
data set for the NH free troposphere and the UT/LMS region. To compare data
from different years a de-trending is applied. In the UT/LMS region
&amp;delta;&lt;sup&gt;13&lt;/sup&gt;C(CO&lt;sub&gt;2&lt;/sub&gt;), &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O(CO&lt;sub&gt;2&lt;/sub&gt;) and CO&lt;sub&gt;2&lt;/sub&gt; are found to
correlate well with stratospheric tracers, in particular N&lt;sub&gt;2&lt;/sub&gt;O. These
correlations are in good agreement with current understanding of
stratospheric circulation. &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O(CO&lt;sub&gt;2&lt;/sub&gt;) appears to be a
useful, hitherto unused, tracer of atmospheric transport in the UT/LMS
region. By filtering out the LMS data (based on N&lt;sub&gt;2&lt;/sub&gt;O distribution), the
isotope variations for the free and upper troposphere are obtained. These
show however little latitudinal gradient, if any, and are in good agreement
with the data of selected NOAA stations in NH tropics. Correlations between
&amp;delta;&lt;sup&gt;13&lt;/sup&gt;C(CO&lt;sub&gt;2&lt;/sub&gt;) and CO&lt;sub&gt;2&lt;/sub&gt; are observed both within single
flight(s) covering long distances and for certain seasons. The overall
variability in de-trended &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C(CO&lt;sub&gt;2&lt;/sub&gt;) and CO&lt;sub&gt;2&lt;/sub&gt; for
CARIBIC-1 and CARIBIC-2 are similar and basically agree with each other,
which also underscores the high quality of measurement. Based on all
correlations, we discuss that CO&lt;sub&gt;2&lt;/sub&gt; distribution in the NH FT and UT (at
CARIBIC flight routes) is regulated by uplift and pole-wards transport of
tropical air up to approximately 50&amp;deg; N. The main reasons for variability
of signals in FT and UT (which is larger for the high spatial resolution
sampling during CARIBIC-2) is mixing of different tropospheric air masses
affected by CO&lt;sub&gt;2&lt;/sub&gt; sources and sinks. The effect of stratospheric flux
appears to be limited. All in all it is demonstrated that CARIBIC produced
new important and reliable data sets for little explored regions of the
atmosphere. A logical next step will be global scale modeling of &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C
and especially &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O, which is linked to the hydrological cycle.</p>
</abstract>
<counts><page-count count="59"/></counts>
</article-meta>
</front>
<body/>
<back>
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