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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>4</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-3699-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/3699/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/3699/2004/acpd-4-3699-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/3699/2004/acpd-4-3699-2004.pdf</fulltext_pdf>
	<start_page>3699</start_page>
	<end_page>3720</end_page>
	<publication_date>2004-07-07</publication_date>
	<article_title content_type="html">Hydroxyl radicals maintain the self-cleansing capacity of the troposphere</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Lelieveld</name>
			<email>lelieveld@mpch-mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>F. J. Dentener</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>W. Peters</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. C. Krol</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, P.O. Box 3060, D-55020 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Joint Research Centre, Institute for Environment and Sustainability, TP280, I-21020 Ispra (Va), Italy</affiliation>
		<affiliation numeration="3" content_type="html">National Oceanic and Atmospheric Administration, Climate Monitoring and Diagnostics Laboratory, 325 Broadway, Boulder, CO 80305, USA</affiliation>
		<affiliation numeration="4" content_type="html">Utrecht University, Institute for Marine and Atmospheric Research, P.O. Box 80005, NL-3508 TA Utrecht, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">Billions of tons natural and anthropogenic gases are released and
subsequently removed from the troposphere each year. Photochemical
reactions, initiated by hydroxyl (OH) radicals, oxidise most gases to
products which are more easily removed by precipitation and dry deposition
at the Earth&apos;s surface. Since human-induced pollution emissions strongly
affect OH formation and loss, large global changes in OH concentrations are
possible. The available evidence as reviewed here, however, indicates that
global mean OH has changed relatively little in the past century. Depletion
of OH by reactive carbon gases has been compensated by increased OH
formation by nitrogen oxides, an act of &amp;quot;inadvertent geo-engineering&amp;quot;.
Analyses of global mean OH for the past 2.5 decades, however, partly based
on methyl chloroform measurements, are ambiguous. Especially the OH trend in
the 1990s based on these analyses is at odds with present understanding.
Since the discrepancy is dominated by the uncertainty in methyl chloroform
emission estimates, improvements of source inventories and model analyses,
combined with continued high precision methyl chloroform measurements, will
help resolve this problem.</abstract>
	<references>
	</references>
</article>

