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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>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-17297-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/17297/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/17297/2008/acpd-8-17297-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/17297/2008/acpd-8-17297-2008.pdf</fulltext_pdf>
	<start_page>17297</start_page>
	<end_page>17341</end_page>
	<publication_date>2008-09-17</publication_date>
	<article_title content_type="html">Investigation of NO&lt;sub&gt;x&lt;/sub&gt; emissions and NO&lt;sub&gt;x&lt;/sub&gt;-related chemistry in East Asia using CMAQ-predicted and GOME-derived NO&lt;sub&gt;2&lt;/sub&gt; columns</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. M. Han</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. H. Song</name>
			<email>chsong@gist.ac.kr</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. J. Ahn</name>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>C. K. Lee</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>A. Richter</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>J. P. Burrows</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>J. Y. Kim</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>J. H. Woo</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>J. H. Hong</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Science and Engineering, Gwangju Institute of Science and Technology (GIST), Gwangju, Korea</affiliation>
		<affiliation numeration="2" content_type="html">Dept. of Physics and Atmospheric Science, Dalhousie Univ., Halifax, Nova Scotia, Canada</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Hazardous Substance Research Center, Korea Institute of Science and Technology (KIST), Seoul, Korea</affiliation>
		<affiliation numeration="5" content_type="html">Dept. of Advanced Technology Fusion, Konkuk University, Seoul, Korea</affiliation>
		<affiliation numeration="6" content_type="html">Air Pollution Cap System Division, National Institute of Environmental Research (NIER), Incheon, Korea</affiliation>
	</affiliations>
	<abstract content_type="html">This study examined the estimation accuracy of NO&lt;sub&gt;x&lt;/sub&gt; emissions over East
Asia with particular focus on North China and South Korea due to their
strong source (North China)-receptor (South Korea) relationship. In order to
determine contributions of North China emissions to South Korean air quality
accurately, it is important to examine the accuracy of the emission
inventories of both regions. In this study, NO&lt;sub&gt;2&lt;/sub&gt; columns from the US EPA
Models-3/CMAQ model simulations carried out using the 2001 ACE-ASIA (Asia
Pacific Regional Aerosol Characterization Experiment) emission inventory
over East Asia were compared with the GOME-derived NO&lt;sub&gt;2&lt;/sub&gt; columns. There
were large discrepancies between the CMAQ-predicted and GOME-derived
NO&lt;sub&gt;2&lt;/sub&gt; columns in the fall and winter seasons. In particular, while the
CMAQ-predicted NO&lt;sub&gt;2&lt;/sub&gt; columns produced larger values than the GOME-derived
NO&lt;sub&gt;2&lt;/sub&gt; columns over South Korea (receptor region) for all four seasons,
the CMAQ-predicted NO&lt;sub&gt;2&lt;/sub&gt; columns produced smaller values than the
GOME-derived NO&lt;sub&gt;2&lt;/sub&gt; columns over North China (source region) for all
seasons with the exception of summer. It is believed that there might be
some estimation error in the NO&lt;sub&gt;x&lt;/sub&gt; emissions as well as large uncertainty
in NO&lt;sub&gt;x&lt;/sub&gt; loss rates over North China and South Korea. Regarding the
latter, this study further focused on the biogenic VOC emissions that were
strongly coupled with NO&lt;sub&gt;x&lt;/sub&gt; chemistry in East Asia. It was found that the
rates of NO&lt;sub&gt;x&lt;/sub&gt; loss determined by CMAQ modeling studies might be
significantly low due to the possible overestimation of biogenic isoprene
emissions during summer, particularly in China. In addition, due to the
possible overestimation of isoprene emissions, the CMAQ-modeled
NO&lt;sub&gt;2&lt;/sub&gt;/NO&lt;sub&gt;x&lt;/sub&gt; ratios might show an incorrectly high level, compared with
the actual NO&lt;sub&gt;2&lt;/sub&gt;/NO&lt;sub&gt;x&lt;/sub&gt; ratios. In addition to the retarded NO&lt;sub&gt;x&lt;/sub&gt;
chemical loss rates and overestimated NO&lt;sub&gt;2&lt;/sub&gt;/NO&lt;sub&gt;x&lt;/sub&gt; ratios, the omission
of soil NO&lt;sub&gt;x&lt;/sub&gt; emissions over North China during summer can lead to an
underestimation of NO&lt;sub&gt;x&lt;/sub&gt; emissions over North China during summer.
Overall, it is estimated that the NO&lt;sub&gt;x&lt;/sub&gt; emissions in North China are
underestimated possibly by ~50% over an entire year. In order to
confirm the uncertainty in NO&lt;sub&gt;x&lt;/sub&gt; emissions, the NO&lt;sub&gt;x&lt;/sub&gt; emission over
South Korea was further investigated using the ACE-ASIA inventory, REAS
(Regional Emission inventory in ASia) and CAPSS (Clean Air Policy Support
System) by NIER (National Institute of Environmental Research) in Korea. The
NO&lt;sub&gt;x&lt;/sub&gt; emissions from ACE-ASIA and the REAS inventories appear to be
approximately 2 times larger for mega-cities in Korea than that from the
CAPSS inventory. In contrast, the NO&lt;sub&gt;x&lt;/sub&gt; emissions of ACE-ASIA and REAS
inventories are only 10% smaller for North China than the
recently-estimated &quot;date-back&quot; ANL (Argonne National Laboratory)
inventory. A comparison between the CMAQ-predicted and GOME-derived NO&lt;sub&gt;2&lt;/sub&gt;
columns indicated that both the ACE-ASIA and REAS inventories have some
uncertainty in NO&lt;sub&gt;x&lt;/sub&gt; emissions over North China (A) and South Korea (C),
which can lead to some error in modeling the formation of ozone and
secondary aerosols in South Korea and North China.</abstract>
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