<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-67-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/67/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/67/2005/acp-5-67-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/67/2005/acp-5-67-2005.pdf</fulltext_pdf>
	<start_page>67</start_page>
	<end_page>75</end_page>
	<publication_date>2005-01-20</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>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Lee</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>K. T. Paw</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>U. 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, 94720-3110, USA</affiliation>
		<affiliation numeration="2" content_type="html">Atmospheric Science Program, Department of Land, Air, and Water Resources, University of California, Davis, California, 95616-8717, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Vertical gradients of mixing ratios of volatile organic compounds have been
measured in a Ponderosa pine forest in Central California (38.90&amp;deg; N,
120.63&amp;deg; W, 1315m). These measurements reveal large quantities of
previously unreported oxidation products of short lived biogenic precursors.
The emission of biogenic precursors must be in the range of 13-66&amp;micro;mol m&lt;sup&gt;-2&lt;/sup&gt;h&lt;sup&gt;-1&lt;/sup&gt;
to produce the observed oxidation products. That is 6-30
times the emissions of total monoterpenes observed above the forest canopy
on a molar basis. These reactive precursors constitute a large 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>

