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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>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-15725-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/15725/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/15725/2009/acpd-9-15725-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/15725/2009/acpd-9-15725-2009.pdf</fulltext_pdf>
	<start_page>15725</start_page>
	<end_page>15746</end_page>
	<publication_date>2009-07-24</publication_date>
	<article_title content_type="html">Increasing synoptic scale variability in atmospheric CO&lt;sub&gt;2&lt;/sub&gt; at Hateruma Island associated with increasing East Asian emissions</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Tohjima</name>
			<email>tohjima@nies.go.jp</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>H. Mukai</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>S. Hashimoto</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>P. K. Patra</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Environment Division, National Institute for Environmental Studies,  Tsukuba, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Japan</affiliation>
		<affiliation numeration="3" content_type="html">Research Institute for Global Change, JAMSTEC, Yokohama, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">In-situ observations of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; at
      Hateruma Island, Japan show large synoptic scale variations
      during a 6-month period from November to April, when the
      sampled air is predominantly of continental origin due to the
      Asian winter monsoon. Synoptic scale variations are extracted
      from the daily averaged values for the years between 1996 and
      2007, along with the annual standard deviations (&amp;sigma;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; and &amp;sigma;&lt;sub&gt;CH&lt;sub&gt;4&lt;/sub&gt;&lt;/sub&gt; for CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt;,
      respectively) for the relevant 6-month period. The temporal
      change in &amp;sigma;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; shows a systematically
      increasing trend over the 12-year period, with elevated
      excursions in 1998 and 2003; there is no clear trend in
      &amp;sigma;&lt;sub&gt;CH&lt;sub&gt;4&lt;/sub&gt;&lt;/sub&gt;. We also find that the &amp;sigma;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;/&amp;sigma;&lt;sub&gt;CH&lt;sub&gt;4&lt;/sub&gt;&lt;/sub&gt; ratio increases gradually from
      1996 to 2002 and rapidly thereafter 2002 without any extreme
      deviations that characterized &amp;sigma;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;. The
      &amp;sigma;&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;/&amp;sigma;&lt;sub&gt;CH&lt;sub&gt;4&lt;/sub&gt;&lt;/sub&gt; ratio correlates
      closely with the recent rapid increase in fossil carbon
      emission from China, as indicated in the CDIAC data. This
      methodology can be applied for tracking overall changes in
      regional emissions by measuring multiple chemical tracers.</abstract>
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</article>

