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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-2289-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/2289/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/2289/2009/acpd-9-2289-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/2289/2009/acpd-9-2289-2009.pdf</fulltext_pdf>
	<start_page>2289</start_page>
	<end_page>2317</end_page>
	<publication_date>2009-01-26</publication_date>
	<article_title content_type="html">Impact of convective transport and lightning NO&lt;sub&gt;x&lt;/sub&gt; production over North America: dependence on cumulus parameterizations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Zhao</name>
			<email>chun.zhao@eas.gatech.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>Y. Wang</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>Y. Choi</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>T. Zeng</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology,  Atlanta, GA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Jet Propulsion Laboratory, Pasadena, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A 3-D regional chemical transport model (REAM) is applied
to examine the uncertainties in modeling the effects of convective transport
and lightning NO&lt;sub&gt;x&lt;/sub&gt; production on upper tropospheric chemical tracer
distributions. To assess the model uncertainties, two different cumulus
convective parameterizations, KF-eta and Grell, are adopted in REAM from the
respective meteorological models, WRF and MM5. The model simulations are
evaluated using INTEX-NA aircraft measurements and satellite measurements of
NO&lt;sub&gt;2&lt;/sub&gt; columns and cloud top pressure, and we find that mid and upper
tropospheric trace gas concentrations are affected strongly by convection
and lightning NO&lt;sub&gt;x&lt;/sub&gt; productions. A major improvement of the KF-eta scheme
is its inclusion of cloud entrainment and detrainment processes. KF-eta
scheme simulates larger convective updraft mass fluxes below 150 hPa than
the Grell scheme, resulting in more outflow of pollutants in the mid
troposphere. The ratio of C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;/C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;8&lt;/sub&gt; is found to be a
sensitive parameter to convective outflow; the simulation by WRF-REAM is in
closer agreement with INTEX-NA measurements than MM5-REAM, implying that
convective mass fluxes by KF-eta scheme are more realistic. The inclusion of
entrainment and detrainment processes in the KF-eta scheme also leads to
lower cloud top heights (10–12 km) than the Grell scheme (up to 16 km), and
hence smaller amounts of estimated (intra-cloud) lightning NO&lt;sub&gt;x&lt;/sub&gt; and
lower emission altitudes. WRF simulated cloud top heights are in better
agreement with GOES satellite measurements than MM5. The model divergence on
lightning NO&lt;sub&gt;x&lt;/sub&gt; mostly is above 12 km. As a result, both models suggest
that lightning NO&lt;sub&gt;x&lt;/sub&gt; production enhances the concentrations of upper
tropospheric NO&lt;sub&gt;2&lt;/sub&gt; by a factor of &gt;5 (~100 pptv) and increases
O&lt;sub&gt;3&lt;/sub&gt; by up to ~20 ppbv at 8–12 km.</abstract>
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</article>

