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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>8</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-8243-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/8243/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/8243/2008/acpd-8-8243-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/8243/2008/acpd-8-8243-2008.pdf</fulltext_pdf>
	<start_page>8243</start_page>
	<end_page>8271</end_page>
	<publication_date>2008-04-25</publication_date>
	<article_title content_type="html">Validation of OMI tropospheric NO&lt;sub&gt;2&lt;/sub&gt; column data using MAX-DOAS measurements deep inside the North China Plain in June 2006</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Irie</name>
			<email>irie@jamstec.go.jp</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>Y. Kanaya</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. Akimoto</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>H. Tanimoto</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>Z. Wang</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>J. F. Gleason</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>E. J. Bucsela</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Frontier Research Center for Global Change, Japan Agency for Marine-Earth Science and Technology, 3173-25 Showa-machi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan</affiliation>
		<affiliation numeration="2" content_type="html">National Inst. for Environmental Studies, 16-2, Onogawa, Tsukuba, Ibaraki 305-8506, Japan</affiliation>
		<affiliation numeration="3" content_type="html">LAPC/NZC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China</affiliation>
		<affiliation numeration="4" content_type="html">Atmospheric Chemistry and Dynamics branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771-0000, USA</affiliation>
		<affiliation numeration="5" content_type="html">SRI International, Menlo Park, CA 94107, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A challenge for the quantitative analysis of tropospheric nitrogen dioxide
(NO&lt;sub&gt;2&lt;/sub&gt;) column data from satellite observations is posed mainly by the
lack of satellite-independent observations for validation. We performed such
observations of the tropospheric NO&lt;sub&gt;2&lt;/sub&gt; column using the ground-based
Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) technique
in the North China Plain (NCP) from 29 May to 29 June 2006. Comparisons
between tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns measured by MAX-DOAS and the Ozone
Monitoring Instrument (OMI) onboard the Aura satellite indicate that OMI
data (the standard product, version 3) over NCP may have a positive bias of
1.6&amp;times;10&lt;sup&gt;15&lt;/sup&gt; molecules cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (20%), where the estimated
random error in the OMI data is 0.6&amp;times;10&lt;sup&gt;15&lt;/sup&gt; molecules cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; or
approximately 8%. Combining these results with literature validation
results for the US, Europe, and Pacific Ocean suggests that a bias of
+20%/&amp;ndash;30% is a reasonable estimate, accounting for different regions.
Considering the uncertainty estimated here will pave the way for
quantitative studies using OMI NO&lt;sub&gt;2&lt;/sub&gt; data, especially over NCP.</abstract>
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</article>

