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<article language="en">
	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>2</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/bg-2-353-2005</doi>
	<article_url>http://www.biogeosciences.net/2/353/2005/</article_url>
	<abstract_html>http://www.biogeosciences.net/2/353/2005/bg-2-353-2005.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/2/353/2005/bg-2-353-2005.pdf</fulltext_pdf>
	<start_page>353</start_page>
	<end_page>375</end_page>
	<publication_date>2005-12-05</publication_date>
	<article_title content_type="html">Inventories of N&lt;sub&gt;2&lt;/sub&gt;O and NO emissions from European forest soils</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Kesik</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. Ambus</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>R. Baritz</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>N. Brüggemann</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>K. Butterbach-Bahl</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. Damm</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>J. Duyzer</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>L. Horváth</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>R. Kiese</name>
		</author>
		<author numeration="10" affiliations="6">
			<name>B. Kitzler</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>A. Leip</name>
		</author>
		<author numeration="12" affiliations="8">
			<name>C. Li</name>
		</author>
		<author numeration="13" affiliations="9">
			<name>M. Pihlatie</name>
		</author>
		<author numeration="14" affiliations="2">
			<name>K. Pilegaard</name>
		</author>
		<author numeration="15" affiliations="7">
			<name>S. Seufert</name>
		</author>
		<author numeration="16" affiliations="10">
			<name>D. Simpson</name>
		</author>
		<author numeration="17" affiliations="11">
			<name>U. Skiba</name>
		</author>
		<author numeration="18" affiliations="1">
			<name>G. Smiatek</name>
		</author>
		<author numeration="19" affiliations="9">
			<name>T. Vesala</name>
		</author>
		<author numeration="20" affiliations="6">
			<name>S. Zechmeister-Boltenstern</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Karlsruhe Research Centre, Institute for Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Kreuzeckbahnstr. 19, 82 467 Garmisch-Partenkirchen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Risoe National Laboratory, Department for Plant Biology and Biogeochemistry, Risø, Denmark</affiliation>
		<affiliation numeration="3" content_type="html">Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany</affiliation>
		<affiliation numeration="4" content_type="html">The Netherlands Organization for Applied Scientific Research, Apeldoorn, Netherlands</affiliation>
		<affiliation numeration="5" content_type="html">Hungarian Meteorological Service, Department for Analysis of Atmospheric Environment, Budapest, Hungary</affiliation>
		<affiliation numeration="6" content_type="html">Federal Forest Research Centre, Institute for Forest Ecology and Soil, Soil Biology, Vienna, Austria</affiliation>
		<affiliation numeration="7" content_type="html">Commission of the European Communities, Environmental Institute, JRC Ispra, Italy</affiliation>
		<affiliation numeration="8" content_type="html">Institute for the Study of Earth, Oceans and Space, Univ. of New Hampshire, Durham, USA</affiliation>
		<affiliation numeration="9" content_type="html">University of Helsinki, Department of Physical Sciences, Helsinki, Finland</affiliation>
		<affiliation numeration="10" content_type="html">Norwegian Meteorology Institute, Oslo, Norway</affiliation>
		<affiliation numeration="11" content_type="html">Natural Environment Research Council, Centre for Ecology and Hydrology, Edinburgh, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Forest soils are a significant source for the primary and secondary
greenhouse gases N&lt;sub&gt;2&lt;/sub&gt;O and NO. However, current estimates are still
uncertain due to the still limited number of field measurements and the
herein observed pronounced variability of N trace gas fluxes in space and
time, which are due to the variation of environmental factors such as soil
and vegetation properties or meteorological conditions. To overcome these
problems we further developed a process-oriented model, the PnET-N-DNDC
model, which simulates the N trace gas exchange on the basis of the
processes involved in production, consumption and emission of N trace gases.
This model was validated against field observations of N trace gas fluxes
from 19 sites obtained within the EU project NOFRETETE, and shown to perform
well for N&lt;sub&gt;2&lt;/sub&gt;O (r&lt;sup&gt;2&lt;/sup&gt;=0.68, slope=0.76) and NO (r&lt;sup&gt;2&lt;/sup&gt;=0.78,
slope=0.73). For the calculation of a European-wide emission inventory we
linked the model to a detailed, regionally and temporally resolved database,
comprising climatic properties (daily resolution), and soil parameters, and
information on forest areas and types for the years 1990, 1995 and 2000. Our
calculations show that N trace gas fluxes from forest soils may vary
substantial from year to year and that distinct regional patterns can be
observed. Our central estimate of NO emissions from forest soils in the EU
amounts to 98.4, 84.9 and 99.2 kt N yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, using meteorology from 1990,
1995 and year 2000, respectively. This is &amp;lt;1.0% of pyrogenic NO&lt;sub&gt;x&lt;/sub&gt;
emissions. For N&lt;sub&gt;2&lt;/sub&gt;O emissions the central estimates were 86.8, 77.6 and
81.6 kt N yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, respectively, which is approx.&amp;nbsp;14.5% of the source
strength coming from agricultural soils. An extensive sensitivity analysis
was conducted which showed a range in emissions from 44.4 to 254.0 kt N yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
for NO and 50.7 to 96.9 kt N yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for N&lt;sub&gt;2&lt;/sub&gt;O, for year 2000
meteorology.
&lt;br /&gt;&lt;br /&gt;
The results show that process-oriented models coupled to a GIS are useful
tools for the calculation of regional, national, or global inventories of
biogenic N trace gas emissions from soils. This work represents the most
comprehensive effort to date to simulate NO and N&lt;sub&gt;2&lt;/sub&gt;O emissions from
European forest soils.</abstract>
	<references>
	</references>
</article>

