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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>6</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-11181-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/11181/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/11181/2006/acpd-6-11181-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/11181/2006/acpd-6-11181-2006.pdf</fulltext_pdf>
	<start_page>11181</start_page>
	<end_page>11207</end_page>
	<publication_date>2006-11-10</publication_date>
	<article_title content_type="html">Systematic analysis of interannual and seasonal variations of model-simulated tropospheric NO&lt;sub&gt;2&lt;/sub&gt; in Asia and comparison with GOME-satellite data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. Uno</name>
			<email>iuno@riam.kyushu-u.ac.jp</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>Y. He</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>T. Ohara</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>K. Yamaji</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>J.-I. Kurokawa</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>M. Katayama</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>Z. Wang</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>K. Noguchi</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>S. Hayashida</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>A. Richter</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>J. P. Burrows</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Research Institute for Applied Mechanics, Kyushu University, Kasuga Park 6-1, Kasuga, Fukuoka, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Earth System Science and Technology, Kyushu University, Kasuga Park 6-1, Kasuga, Fukuoka, Japan</affiliation>
		<affiliation numeration="3" content_type="html">National Institute for Environmental Studies, Tsukuba, Ibaraki, Japan</affiliation>
		<affiliation numeration="4" content_type="html">Frontier Research Center for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan</affiliation>
		<affiliation numeration="5" content_type="html">NZC/LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China</affiliation>
		<affiliation numeration="6" content_type="html">Information Science, Faculty of Science, Nara Women’s University, Nara, Japan</affiliation>
		<affiliation numeration="7" content_type="html">Institute of Environmental Physics, University of Bremen, Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Systematic analyses of interannual and seasonal variations of tropospheric
NO&lt;sub&gt;2&lt;/sub&gt; vertical column densities (VCDs) based on GOME satellite data and
the regional scale chemical transport model (CTM), Community Multi-scale Air
Quality (CMAQ), are presented over eastern Asia between 1996 and June 2003.
A newly developed year-by-year emission inventory (REAS) was used in CMAQ.
The horizontal distribution of annual averaged GOME NO&lt;sub&gt;2&lt;/sub&gt; VCDs generally
agrees well with the CMAQ results. However, CMAQ/REAS results underestimate
the GOME retrievals with factors of 2&amp;ndash;4 over polluted industrial regions
such as Central East China (CEC), a major part of Korea, Hong Kong, and
central and western Japan. For the Japan region, GOME and CMAQ NO&lt;sub&gt;2&lt;/sub&gt; data
show good agreement with respect to interannual variation and show no clear
increasing trend. For CEC, GOME and CMAQ NO&lt;sub&gt;2&lt;/sub&gt; data show good agreement
and indicate a very rapid increasing trend from 2000. Analyses of the
seasonal cycle of NO&lt;sub&gt;2&lt;/sub&gt; VCDs show that GOME data have systematically
larger dips than CMAQ NO&lt;sub&gt;2&lt;/sub&gt; during February&amp;ndash;April and
September&amp;ndash;November. Sensitivity experiments with fixed emission intensity
reveal that the detection of emission trends from satellite in fall or
winter have a larger error caused by the variability of meteorology.
Examination during summer time and annual averaged NO&lt;sub&gt;2&lt;/sub&gt; VCDs are robust
with respect to variability of meteorology and are therefore more suitable
for analyses of emission trends. Analysis of recent trends of annual
emissions in China shows that the increasing trends of 1996&amp;ndash;1998 and
2000&amp;ndash;2002 for GOME and CMAQ/REAS show good agreement, but the rate of
increase by GOME is approximately 10&amp;ndash;11% yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; after 2000; it
is slightly steeper than CMAQ/REAS (8&amp;ndash;9% yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;). The greatest
difference was apparent between the years 1998 and 2000: CMAQ/REAS only
shows a few percentage points of increase, whereas GOME gives a greater than
8% yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; increase. The exact reason remains unclear, but the
most likely explanation is that the emission trend based on the Chinese
emission related statistics underestimates the rapid growth of emissions.</abstract>
	<references>
	</references>
</article>

