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	<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>7</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-4705-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/4705/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/4705/2007/acpd-7-4705-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/4705/2007/acpd-7-4705-2007.pdf</fulltext_pdf>
	<start_page>4705</start_page>
	<end_page>4760</end_page>
	<publication_date>2007-04-05</publication_date>
	<article_title content_type="html">Wildfire particulate matter in Europe during summer 2003: meso-scale modeling of smoke emissions, transport and radiative effects</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Hodzic</name>
			<email>alma@ucar.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Madronich</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>B. Bohn</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>S. Massie</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>L. Menut</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>C. Wiedinmyer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Center for Atmospheric Research, Atmospheric Chemistry Division, Boulder CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Forschungszentrum Juelich, ICG Institut II: Troposphere, 52425 Juelich, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Institut Pierre-Simon Laplace, Ecole Polytechnique, Palaiseau, France</affiliation>
	</affiliations>
	<abstract content_type="html">The present study investigates effects of wildfire emissions on air quality
in Europe during an intense fire season that occurred in summer 2003. A
meso-scale chemistry transport model CHIMERE is used, together with ground
based and satellite aerosol optical measurements, to assess the dispersion
of fire emissions and to quantify the associated radiative effects. The
model has been improved to take into account the MODIS daily smoke emission
inventory as well as the injection altitude of smoke particles. The
simulated aerosol optical properties are inputted into a radiative transfer
model to estimate (off-line) the effects of smoke particles on photolysis
rates and atmospheric radiative forcing. We have found that wildfires
generated comparable amounts of primary aerosol pollutants (220 kTons of
PM&lt;sub&gt;2.5&lt;/sub&gt;, fine particles) to anthropogenic sources during August 2003, and
caused significant changes in aerosol optical properties not only close to
the fire source regions, but also over a large part of Europe as a result of
the long-range transport of smoke. Including these emissions into the model
significantly improved its performance in simulating observed aerosol
concentrations and optical properties. Quantitative comparison with MODIS
and POLDER data during the major fire event (3&amp;ndash;8 August) showed the ability
of the model to reproduce high aerosol optical thickness (AOT) over Northern
Europe caused by the advection of the smoke plume from the Portugal source
region. Statistical analyses of model simulations showed a better agreement
with observed AOT data at AERONET ground stations and suggest that wildfire
emissions are responsible for a 30% enhancement in mean AOT values during
the heat-wave episode. The implications for air quality over a large part of
Europe are significant during this episode. First, directly, the modeled
wildfire emissions caused an increase in average PM&lt;sub&gt;10&lt;/sub&gt; ground
concentrations from 20 to 200%. The largest enhancement in PM&lt;sub&gt;10&lt;/sub&gt;
concentrations stayed however confined within a 200 km area around the fire
source locations and reached up to 40 &amp;mu; g/m&lt;sup&gt;3&lt;/sup&gt;. Second, indirectly,
the presence of elevated smoke layers over Europe significantly altered
atmospheric radiative properties: the model results imply a 10 to 30%
decrease in photolysis rates and an increase in atmospheric radiative
forcing of 10&amp;ndash;35 Wm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; during the period of strong fire influence
throughout a large part of Europe. These results suggest that sporadic
wildfire events may have significant effects on regional photochemistry and
atmospheric stability, and need to be considered in current
chemistry-transport models.</abstract>
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