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	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>7</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bg-7-1991-2010</doi>
	<article_url>http://www.biogeosciences.net/7/1991/2010/</article_url>
	<abstract_html>http://www.biogeosciences.net/7/1991/2010/bg-7-1991-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/7/1991/2010/bg-7-1991-2010.pdf</fulltext_pdf>
	<start_page>1991</start_page>
	<end_page>2011</end_page>
	<publication_date>2010-06-23</publication_date>
	<article_title content_type="html">The influence of vegetation, fire spread and fire behaviour on biomass burning and trace gas emissions: results from a process-based model</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,3,9">
			<name>K. Thonicke</name>
			<email>kirsten.thonicke@pik-potsdam.de</email>
		</author>
		<author numeration="2" affiliations="1,4">
			<name>A. Spessa</name>
		</author>
		<author numeration="3" affiliations="1,5,6,7">
			<name>I. C. Prentice</name>
		</author>
		<author numeration="4" affiliations="2,6">
			<name>S. P. Harrison</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>L. Dong</name>
		</author>
		<author numeration="6" affiliations="8">
			<name>C. Carmona-Moreno</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">formerly Max Planck Institute for Biogeochemistry, Hans-Knöll-Straße 10, Jena, 07701, Germany</affiliation>
		<affiliation numeration="2" content_type="html">School of Geographical Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK</affiliation>
		<affiliation numeration="3" content_type="html">Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia</affiliation>
		<affiliation numeration="4" content_type="html">Grantham Institute for Climate Change, and Division of Biology, Imperial College, Silwood Park Campus, Ascot, SL5 7PY, UK</affiliation>
		<affiliation numeration="5" content_type="html">Potsdam Institute for Climate Impact Research (PIK) e.V., Telegraphenberg A31, Potsdam, 14473, Germany</affiliation>
		<affiliation numeration="6" content_type="html">National Centre for Atmospheric Sciences (NCAS), NCAS-Climate, University of Reading, Earley Gate, Reading, RG6 6BB, UK</affiliation>
		<affiliation numeration="7" content_type="html">QUEST, Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen&apos;s Road, Bristol, BS8 1RJ, UK</affiliation>
		<affiliation numeration="8" content_type="html">Global Vegetation Monitoring Unit, Joint Research Centre Ispra, Ispra, Italy</affiliation>
		<affiliation numeration="9" content_type="html">now at: Potsdam Institute for Climate Impact Research (PIK) e.V., Telegraphenberg A31, Potsdam, 14473, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A process-based fire regime model (SPITFIRE) has been developed, coupled
with ecosystem dynamics in the LPJ Dynamic Global Vegetation Model, and used
to explore fire regimes and the current impact of fire on the terrestrial
carbon cycle and associated emissions of trace atmospheric constituents. The
model estimates an average release of 2.24 Pg C yr&lt;sup&gt;−1&lt;/sup&gt; as CO&lt;sub&gt;2&lt;/sub&gt; from
biomass burning during the 1980s and 1990s. Comparison with observed active
fire counts shows that the model reproduces where fire occurs and can mimic
broad geographic patterns in the peak fire season, although the predicted
peak is 1–2 months late in some regions. Modelled fire season length is
generally overestimated by about one month, but shows a realistic pattern of
differences among biomes. Comparisons with remotely sensed burnt-area
products indicate that the model reproduces broad geographic patterns of
annual fractional burnt area over most regions, including the boreal forest,
although interannual variability in the boreal zone is underestimated.</abstract>
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</article>

