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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-4-5345-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/5345/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/5345/2004/acpd-4-5345-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/5345/2004/acpd-4-5345-2004.pdf</fulltext_pdf>
	<start_page>5345</start_page>
	<end_page>5365</end_page>
	<publication_date>2004-09-15</publication_date>
	<article_title content_type="html">Observations of oxidation products above a forest imply biogenic emissions of very reactive compounds</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Holzinger</name>
			<email>holzing@nature.berkeley.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Lee</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>K. T. Paw U</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>A. H. Goldstein</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Science, Policy, and Management (ESPM), Division of Ecosystem Sciences, University of California, Berkeley, California, USA</affiliation>
		<affiliation numeration="2" content_type="html">Atmospheric Science Program, Department of Land, Air, and Water Resources, University of California, Davis, California, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of volatile organic compounds in a pine forest (Central
California, 38.90&amp;deg; N, 120.63&amp;deg; W, 1315 m) reveal large quantities of
previously unreported oxidation products of short lived biogenic precursors.
The emission of biogenic precursors must be in the range of 13&amp;ndash;66 &amp;micro;mol&amp;nbsp;m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;&amp;nbsp;h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
to produce the observed oxidation products. That is 6&amp;ndash;30
times the emissions of total monoterpenes observed above the forest canopy
on a molar basis. These reactive precursors constitute the largest fraction
of biogenic emissions at this site, and are not included in current emission
inventories. When oxidized by ozone they should efficiently produce
secondary aerosol and hydroxyl radicals.</abstract>
	<references>
	</references>
</article>

