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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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-18201-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/18201/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/18201/2009/acpd-9-18201-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/18201/2009/acpd-9-18201-2009.pdf</fulltext_pdf>
	<start_page>18201</start_page>
	<end_page>18233</end_page>
	<publication_date>2009-09-02</publication_date>
	<article_title content_type="html">Wildfire smoke in the Siberian Arctic in summer: source characterization and plume evolution from airborne measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-D. Paris</name>
			<email>jean-daniel.paris@lsce.ipsl.fr</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Stohl</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P. Nédélec</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. Yu. Arshinov</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>M. V. Panchenko</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>V. P. Shmargunov</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>K. S. Law</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>B. D. Belan</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>P. Ciais</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement/IPSL, CNRS-CEA-UVSQ, Orme des Merisiers, CEA Saclay, Gif sur Yvette, France</affiliation>
		<affiliation numeration="2" content_type="html">Norwegian Institute for Air Research, Kjeller, Norway</affiliation>
		<affiliation numeration="3" content_type="html">Laboratoire d&apos;Aérologie, CNRS-UPS, Toulouse, France</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Atmospheric Optics, SB-RAS, Tomsk, Russia</affiliation>
		<affiliation numeration="5" content_type="html">UPMC Univ. Paris 06; Univ. Versailles St-Quentin; CNRS/INSU, LATMOS-IPSL, Paris, France</affiliation>
	</affiliations>
	<abstract content_type="html">We present airborne measurements of carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;),
      carbon monoxide (CO), ozone (O&lt;sub&gt;3&lt;/sub&gt;), equivalent black carbon
      (EBC) and ultra fine particles over North-Eastern Siberia in
      July 2008 performed during the YAK-AEROSIB/POLARCAT
      experiment. During a &quot;golden day&quot; (11 July 2008) a number of
      biomass burning plumes were encountered with CO concentration
      enhancements of up to 500 ppb relative to a background of
      90 ppb. Number concentrations of aerosols in the size range
      3.5–200 nm peaked at 4000 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and the EBC content
      reached 1.4 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. These high concentrations were
      caused by forest fires in the vicinity of the landing airport
      in Yakutsk where during the descent measurements in fresh
      smoke could be made. We estimate a combustion efficiency of
      90&amp;plusmn;3% based on CO and CO&lt;sub&gt;2&lt;/sub&gt; measurements. The
      emission factor of CO emitted was 59.6&amp;plusmn;15.2 g CO per
      kilogram of dry matter burned, suggesting an increase in the
      average northern hemispheric CO concentration of 3.0–7.2 ppb
      per million hectares of Siberian forest burned. For BC, we
      estimate an emission factor of 0.52&amp;plusmn;0.07 g BC kg&lt;sup&gt;&amp;minus;1&lt;/sup&gt;,
      comparable to values reported in the literature. The emission
      ratio of ultra-fine particles (3.5–200 nm) was 26 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
      (ppb CO)&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, consistent with other airborne studies.

&lt;br&gt;&lt;br&gt;

      The transport of identified biomass burning plumes was
      investigated using the FLEXPART Lagrangian model. Based on
      sampling of wildfire plumes from the same source but with
      different atmospheric ages derived from FLEXPART, we estimate
      that the e-folding lifetimes of EBC and ultra fine particles (between 3.5 and 200 nm in size) against removal and growth processes
are 5.1 and 5.5 days, respectively, supporting lifetimes estimates used in various
      modelling studies.</abstract>
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</article>

