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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-3401-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/3401/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/3401/2010/acpd-10-3401-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/3401/2010/acpd-10-3401-2010.pdf</fulltext_pdf>
	<start_page>3401</start_page>
	<end_page>3421</end_page>
	<publication_date>2010-02-09</publication_date>
	<article_title content_type="html">CO&lt;sub&gt;2&lt;/sub&gt; column-averaged volume mixing ratio derived over Tsukuba from measurements by commercial airlines</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>M. Araki</name>
			<email>araki@rs.kagu.tus.ac.jp</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>I. Morino</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Machida</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>Y. Sawa</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>H. Matsueda</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>T. Yokota</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>O. Uchino</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, baraki 305-8506, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Meteorological Research Institute, 1-1 Nagamine, Tsukuba 305-0052, Japan</affiliation>
		<affiliation numeration="3" content_type="html">now at: Department of Chemistry, Faculty of Science Division I, Tokyo University of Science, 1-3 Kagurazaka, Shinjuku-ku, Tokyo 162-8601, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">Column-averaged volume mixing ratios of carbon dioxide
      (&lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;) during the period from January 2007 to May 2008
      over Tsukuba, Japan, were derived by using CO&lt;sub&gt;2&lt;/sub&gt; concentration
      data observed by Japan Airlines Corporation (JAL) commercial
      airliners, based on the assumption that CO&lt;sub&gt;2&lt;/sub&gt; profiles over
      Tsukuba and Narita were the same. CO&lt;sub&gt;2&lt;/sub&gt; profile data for 493
      flights on clear-sky days were analysed in order to calculate
&lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; with an ancillary dataset: Tsukuba observational
      data (by rawinsonde and a meteorological tower) or global
      meteorological data (NCEP and CIRA-86). The amplitude of seasonal
      variation of &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (Tsukuba observational) from the
      Tsukuba observational data was determined by least-squares fit using
      a harmonic function to roughly evaluate the seasonal variation over
      Tsukuba. The highest and lowest values of the obtained fitted curve in
      2007 for &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (Tsukuba observational) were 386.4 and
      381.7 ppm in May and September, respectively. The dependence of
&lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; on the type of ancillary dataset was evaluated. The
      average difference between &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (global) from global
      climatological data and &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (Tsukuba observational),
      i.e., the bias of &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (global) based on
&lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (Tsukuba observational), was found to be
-0.621 ppm with a standard deviation of 0.682 ppm. The
      uncertainty of &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; (global) based on &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;
      (Tsukuba observational) was estimated to be 0.922 ppm. This small
      uncertainty suggests that the present method of &lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;
      calculation using data from airliners and global climatological data
      can be applied to the validation of GOSAT products for
&lt;i&gt;X&lt;/i&gt;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; over airports worldwide.</abstract>
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