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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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-1797-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/1797/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/1797/2005/acpd-5-1797-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/1797/2005/acpd-5-1797-2005.pdf</fulltext_pdf>
	<start_page>1797</start_page>
	<end_page>1828</end_page>
	<publication_date>2005-03-21</publication_date>
	<article_title content_type="html">Modelling photochemistry in alpine valleys</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Brulfert</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. Chemel</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>E. Chaxel</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. P. Chollet</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory of Geophysical and industrial Fluid Flows, University J. Fourier, INP Grenoble, CNRS, BP53, 38041 Grenoble cedex, France</affiliation>
	</affiliations>
	<abstract content_type="html">Road traffic is a serious problem in the Chamonix Valley, France: traffic,
noise and above all air pollution worry the inhabitants. The big fire in the
Mont-Blanc tunnel made it possible, in the framework of the POVA project
(POllution in Alpine Valleys), to undertake measurement campaigns with and
without heavy-vehicle traffic through the valley, towards Italy (before and
after the tunnel re-opening). Modelling in POVA should make it possible to
explain the processes leading to episodes of atmospheric pollution, both in
summer and in winter.
&lt;br&gt;&lt;br&gt;
Atmospheric prediction model ARPS 4.5.2 (Advanced Regional Prediction
System), developed at the CAPS (Center for Analysis and Prediction of
Storms) of the University of Oklahoma, enables to resolve the dynamics above
a complex terrain.
&lt;br&gt;&lt;br&gt;
This model is coupled to the TAPOM 1.5.2 atmospheric chemistry (Transport
and Air POllution Model) code developed at the Air and Soil Pollution
Laboratory of the Ecole Polytechnique F&amp;#233;d&amp;#233;rale de Lausanne.
&lt;br&gt;&lt;br&gt;
The numerical codes MM5 and CHIMERE are used to compute large scale boundary
forcing.
&lt;br&gt;&lt;br&gt;
Using 300-m grid cells to calculate the dynamics and the reactive
chemistry makes possible to accurately represent the dynamics in the valley
(slope and valley winds) and to process chemistry at fine scale.
&lt;br&gt;&lt;br&gt;
Validation of campaign days allows to study chemistry indicators in the
valley. NO&lt;sub&gt;y&lt;/sub&gt; according to O&lt;sub&gt;3&lt;/sub&gt; reduction demonstrates a VOC controlled
regime, different from the NO&lt;sub&gt;x&lt;/sub&gt; controlled regime expected and observed in
the nearby city of Grenoble.</abstract>
	<references>
	</references>
</article>

