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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-9-767-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/767/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/767/2009/acpd-9-767-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/767/2009/acpd-9-767-2009.pdf</fulltext_pdf>
	<start_page>767</start_page>
	<end_page>835</end_page>
	<publication_date>2009-01-09</publication_date>
	<article_title content_type="html">Emissions from biomass burning in the Yucatan</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Yokelson</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. D. Crounse</name>
		</author>
		<author numeration="3" affiliations="3,4">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="4" affiliations="5">
			<name>T. Karl</name>
		</author>
		<author numeration="5" affiliations="6">
			<name>S. Urbanski</name>
		</author>
		<author numeration="6" affiliations="7">
			<name>E. Atlas</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>T. Campos</name>
		</author>
		<author numeration="8" affiliations="8">
			<name>Y. Shinozuka</name>
		</author>
		<author numeration="9" affiliations="8">
			<name>V. Kapustin</name>
		</author>
		<author numeration="10" affiliations="8">
			<name>A. D. Clarke</name>
		</author>
		<author numeration="11" affiliations="5">
			<name>A. Weinheimer</name>
		</author>
		<author numeration="12" affiliations="5">
			<name>D. J. Knapp</name>
		</author>
		<author numeration="13" affiliations="5">
			<name>D. D. Montzka</name>
		</author>
		<author numeration="14" affiliations="9">
			<name>J. Holloway</name>
		</author>
		<author numeration="15" affiliations="5">
			<name>P. Weibring</name>
		</author>
		<author numeration="16" affiliations="5">
			<name>F. Flocke</name>
		</author>
		<author numeration="17" affiliations="5">
			<name>W. Zheng</name>
		</author>
		<author numeration="18" affiliations="10">
			<name>D. Toohey</name>
		</author>
		<author numeration="19" affiliations="11">
			<name>P. O. Wennberg</name>
		</author>
		<author numeration="20" affiliations="5">
			<name>C. Wiedinmyer</name>
		</author>
		<author numeration="21" affiliations="5">
			<name>L. Mauldin</name>
		</author>
		<author numeration="22" affiliations="5">
			<name>A. Fried</name>
		</author>
		<author numeration="23" affiliations="5">
			<name>D. Richter</name>
		</author>
		<author numeration="24" affiliations="5">
			<name>J. Walega</name>
		</author>
		<author numeration="25" affiliations="12">
			<name>J. L. Jimenez</name>
		</author>
		<author numeration="26" affiliations="13">
			<name>K. Adachi</name>
		</author>
		<author numeration="27" affiliations="13">
			<name>P. R. Buseck</name>
		</author>
		<author numeration="28" affiliations="5">
			<name>S. R. Hall</name>
		</author>
		<author numeration="29" affiliations="5">
			<name>R. Shetter</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Montana, Department of Chemistry, Missoula, MT 59812, USA</affiliation>
		<affiliation numeration="2" content_type="html">Division of Chemistry and Chemical Engineering, California Institute  of Technology, Pasadena, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Colorado, Cooperative Institute for Research in the  Environmental Sciences (CIRES), and Department of Atmospheric and Oceanic  Sciences, Boulder, USA</affiliation>
		<affiliation numeration="4" content_type="html">Now at the Paul Scherrer Institut, Villigen Switzerland</affiliation>
		<affiliation numeration="5" content_type="html">National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
		<affiliation numeration="6" content_type="html">USDA Forest Service, Fire Sciences Laboratory, Missoula, MT, USA</affiliation>
		<affiliation numeration="7" content_type="html">University of Miami, Rosenstiel School of Marine and Atmospheric  Science, USA</affiliation>
		<affiliation numeration="8" content_type="html">School of Ocean and Earth Sciences and Department of Oceanography,  University of Hawaii, Honolulu, USA</affiliation>
		<affiliation numeration="9" content_type="html">NOAA ESRL/CSD, Boulder, CO, USA</affiliation>
		<affiliation numeration="10" content_type="html">University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, USA</affiliation>
		<affiliation numeration="11" content_type="html">Divisions of Engineering and Applied Science and Geological and Planetary Science, California Institute of Technology, Pasadena, USA</affiliation>
		<affiliation numeration="12" content_type="html">University of Colorado, Cooperative Institute for Research in the Environmental Sciences (CIRES) and Department of Chemistry and Biochemistry, Boulder, USA</affiliation>
		<affiliation numeration="13" content_type="html">School of Earth and Space Exploration and Department of Chemistry and Biochemistry, Arizona, State University, Tempe, USA</affiliation>
	</affiliations>
	<abstract content_type="html">In March 2006 two instrumented aircraft made the first detailed field
measurements of biomass burning (BB) emissions in the Northern Hemisphere
tropics as part of the MILAGRO project. The aircraft were the National Center
for Atmospheric Research C-130 and a University of Montana/US Forest Service
Twin Otter. The initial emissions of up to 49 trace gas or particle species
were measured from 20 deforestation and crop residue fires on the Yucatan
peninsula. This included two trace gases useful as indicators of BB (HCN and
acetonitrile) and several rarely, or never before, measured species: OH,
peroxyacetic acid, propanoic acid, hydrogen peroxide, methane sulfonic acid,
and sulfuric acid. Crop residue fires emitted more organic acids and ammonia
than deforestation fires, but the emissions from the main fire types were
otherwise fairly similar. The Yucatan fires emitted unusually high amounts of
SO&lt;sub&gt;2&lt;/sub&gt; and particle chloride, likely due to a strong marine influence on
this peninsula. As smoke from one fire aged, the ratio &amp;Delta;O&lt;sub&gt;3&lt;/sub&gt;/&amp;Delta;CO increased to ~15% in &lt;~1 h
similar to the fast net production of O&lt;sub&gt;3&lt;/sub&gt; in BB plumes
observed earlier in Africa. The rapid change in O&lt;sub&gt;3&lt;/sub&gt; occurs at a finer
spatial scale than is employed in global models and is also faster than
predicted by micro-scale models. Fast increases in PAN, H&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt;, and two
organic acids were also observed. The amount of secondary organic acid is
larger than the amount of known precursors. Rapid secondary formation of
organic and inorganic aerosol was observed with the ratio &amp;Delta;PM&lt;sub&gt;2.5&lt;/sub&gt;/&amp;Delta;CO more than doubling in ~1.4&amp;plusmn0.7 h.
The OH measurements revealed high initial OH levels &gt;1&amp;times;10&lt;sup&gt;7&lt;/sup&gt; molecules/cm&lt;sup&gt;3&lt;/sup&gt;. Thus, more research is needed to
understand critical post emission processes for the second-largest trace gas
source on Earth. It is estimated that ~44 Tg of biomass burned
in the Yucatan in the spring of 2006. Mexican BB (including Yucatan BB) and
urban emissions from the Mexico City area can both influence the March–May air
quality in much of Mexico and the US.</abstract>
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</article>

