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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-12-3393-2012</article-id>
<title-group>
<article-title>Influence of aerosols and thin cirrus clouds on the GOSAT-observed CO&lt;sub&gt;2&lt;/sub&gt;: a case study over Tsukuba</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Uchino</surname>
<given-names>O.</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>Kikuchi</surname>
<given-names>N.</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>Sakai</surname>
<given-names>T.</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>Morino</surname>
<given-names>I.</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>Yoshida</surname>
<given-names>Y.</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>Nagai</surname>
<given-names>T.</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>Shimizu</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>Shibata</surname>
<given-names>T.</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>Yamazaki</surname>
<given-names>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>Uchiyama</surname>
<given-names>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>Kikuchi</surname>
<given-names>N.</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>Oshchepkov</surname>
<given-names>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>Bril</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>Yokota</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki 305-8506, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Meteorological Research Institute, 1-1 Nagamine, Tsukuba, Ibaraki 305-0052, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Graduate School of Environmental Studies, Nagoya University, D2-1(510) Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>7</issue>
<fpage>3393</fpage>
<lpage>3404</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/12/3393/2012/acp-12-3393-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/3393/2012/acp-12-3393-2012.pdf</self-uri>
<abstract>
<p>Lidar observations of vertical profiles of aerosols and thin cirrus clouds
were made at Tsukuba (36.05Â° N, 140.12Â° E), Japan, to
investigate the influence of aerosols and thin cirrus clouds on the
column-averaged dry-air mole fraction of carbon dioxide (XCO&lt;sub&gt;2&lt;/sub&gt;) retrieved
from observation data of the Thermal And Near-infrared Sensor for carbon
Observation Fourier Transform Spectrometer, measured in the Short-Wavelength
InfraRed band (TANSO-FTS SWIR), onboard the Greenhouse gases Observing
SATellite (GOSAT). The lidar system measured the backscattering ratio,
depolarization ratio, and/or the wavelength exponent of atmospheric
particles. The lidar observations and ground-based high-resolution FTS
measurements at the Tsukuba Total Carbon Column Observing Network (Tsukuba
TCCON) site were recorded simultaneously during passages of GOSAT over
Tsukuba.
&lt;br&gt;&lt;/br&gt;
GOSAT SWIR XCO&lt;sub&gt;2&lt;/sub&gt; data (Version 01.xx) released in August 2010 were
compared with the lidar and Tsukuba TCCON data. High-altitude aerosols and
thin cirrus clouds had a large impact on the GOSAT SWIR XCO&lt;sub&gt;2&lt;/sub&gt; results. By
taking into account the observed aerosol/cirrus vertical profiles and using a
more adequate solar irradiance database in the GOSAT SWIR retrieval, the
difference between the GOSAT SWIR XCO&lt;sub&gt;2&lt;/sub&gt; data and the Tsukuba TCCON data
was reduced. The 3-band retrieval approach where the aerosol and cirrus
profiles were retrieved gave us the best results and the retrieved XCO&lt;sub&gt;2&lt;/sub&gt;
data followed the seasonal cycle of ~8 ppm observed at Tsukuba TCCON
site.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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