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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-10-5601-2010</article-id>
<title-group>
<article-title>Characterization of Tropospheric Emission Spectrometer (TES) CO&lt;sub&gt;2&lt;/sub&gt; for carbon cycle science</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulawik</surname>
<given-names>S. 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>Jones</surname>
<given-names>D. B. A.</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>Nassar</surname>
<given-names>R.</given-names>
</name>
<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>Irion</surname>
<given-names>F. W.</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>Worden</surname>
<given-names>J. R.</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>Bowman</surname>
<given-names>K. W.</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>Machida</surname>
<given-names>T.</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>Matsueda</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sawa</surname>
<given-names>Y.</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>Biraud</surname>
<given-names>S. C.</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>Fischer</surname>
<given-names>M. L.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jacobson</surname>
<given-names>A. R.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA, 91109, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Toronto, Department of Physics, Toronto, Ontario, Canada</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Toronto, Department of Geography, Toronto, Ontario, Canada</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Institute for Environmental studies, 16-2 Onogawa, Tsukuba-City, Ibaraki, 305-8506, Japan</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Meteorological Research Institute, 1-1 Nagamine, Tsukuba-City, Ibaraki, 305-0052, Japan</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Lawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>E. O. Lawrence Berkeley National Laboratory, Environmental Energy Technologies Division, Berkeley, CA, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>NOAA Earth System Research Lab, Global Monitoring Division, Boulder, Colorado, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>06</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>12</issue>
<fpage>5601</fpage>
<lpage>5623</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/5601/2010/acp-10-5601-2010.html">This article is available from http://www.atmos-chem-phys.net/10/5601/2010/acp-10-5601-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/5601/2010/acp-10-5601-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/5601/2010/acp-10-5601-2010.pdf</self-uri>
<abstract>
<p>We present carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) estimates from the Tropospheric
Emission Spectrometer (TES) on the EOS-Aura satellite launched in 2004. For
observations between 40° S and 45° N, we find about 1 degree of
freedom with peak sensitivity at 511 hPa. The estimated error is ~10 ppm
for a single target and 1.3–2.3 ppm for monthly averages on spatial
scales of 20&amp;deg;&amp;times;30°. Monthly spatially-averaged TES data from
2005–2008 processed with a uniform initial guess and prior are compared to
CONTRAIL aircraft data over the Pacific ocean, aircraft data at the Southern
Great Plains (SGP) ARM site in the southern US, and the Mauna Loa and
Samoa surface stations. Comparisons to Mauna Loa data show a correlation of
0.92, a standard deviation of 1.3 ppm, a predicted error of 1.2 ppm, and a
~2% low bias, which is subsequently corrected. Comparisons to SGP
aircraft data over land show a correlation of 0.67 and a standard deviation
of 2.3 ppm. TES data between 40° S and 45° N for 2006–2007 are
compared to surface flask data, GLOBALVIEW, the Atmospheric Infrared Sounder
(AIRS), and CarbonTracker. Comparison to GLOBALVIEW-CO&lt;sub&gt;2&lt;/sub&gt; ocean surface
sites shows a correlation of 0.60 which drops when TES is offset in
latitude, longitude, or time. At these same locations, TES shows a 0.62 and
0.67 correlation to CarbonTracker at the surface and 5 km, respectively. We
also conducted an observing system simulation experiment to assess the
potential utility of the TES data for inverse modeling of CO&lt;sub&gt;2&lt;/sub&gt; fluxes.
We find that if biases in the data and model are well characterized, the
averaged data have the potential to provide sufficient information to
significantly reduce uncertainty on annual estimates of regional CO&lt;sub&gt;2&lt;/sub&gt;
sources and sinks. Averaged pseudo-data at 10&amp;deg;&amp;times;10° reduced
uncertainty in flux estimates by as much as 70% for some tropical regions.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
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