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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>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-6321-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/6321/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/6321/2004/acpd-4-6321-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/6321/2004/acpd-4-6321-2004.pdf</fulltext_pdf>
	<start_page>6321</start_page>
	<end_page>6340</end_page>
	<publication_date>2004-10-07</publication_date>
	<article_title content_type="html">Oxygenated compounds in aged biomass burning plumes over the Eastern Mediterranean: evidence for strong secondary production of methanol and acetone</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>R. Holzinger</name>
			<email>holzing@nature.berkeley.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Williams</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>G. Salisbury</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>T. Klüpfel</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. de Reus</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. Traub</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>P. J. Crutzen</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>J. Lelieveld</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max-Planck-Institut für Chemie, Postfach 3060, 55020 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">now at: University of California at Berkeley, Dept. Environm. Sci. Policy and Management, Berkeley, CA 94720, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Airborne measurements of acetone, methanol, PAN, acetonitrile (by Proton
Transfer Reaction Mass Spectrometry), and CO (by Tunable Diode Laser
Absorption Spectroscopy) have been performed during the Mediterranean
Intensive Oxidants Study (MINOS, August 2001). In the course of the campaign
10 biomass burning plumes, identified by strongly elevated acetonitrile
mixing ratios, were found. The characteristic biomass burning signatures
obtained from these plumes reveal secondary production of acetone and
methanol, while CO photochemically declines in the plumes. Mean excess
mixing ratios &amp;ndash; normalized to CO &amp;ndash; of 1.8%, 0.20%, 3.8%, and
0.65% for acetone, acetonitrile, methanol, and PAN, respectively, were
found in the plumes. By scaling to an assumed global annual source of
663&amp;ndash;807 Tg CO, biomass burning emissions of 25&amp;ndash;31 and 29&amp;ndash;35 Tg/yr for
acetone and methanol are estimated, respectively. Our measurements suggest
that the present biomass burning contributions of acetone and methanol are
significantly underestimated due to the neglect of secondary formation.
Median acetonitrile mixing ratios throughout the troposphere were around
150 pmol/mol; this is in accord with current biomass burning inventories and an
atmospheric lifetime of ~6&amp;nbsp;months.</abstract>
	<references>
	</references>
</article>

