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<!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>9</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-2431-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/2431/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/2431/2005/acp-5-2431-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/2431/2005/acp-5-2431-2005.pdf</fulltext_pdf>
	<start_page>2431</start_page>
	<end_page>2460</end_page>
	<publication_date>2005-09-21</publication_date>
	<article_title content_type="html">Inverse modelling of national and European CH&lt;sub&gt;4&lt;/sub&gt; emissions using the atmospheric zoom model TM5</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Bergamaschi</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Krol</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. Dentener</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>A. Vermeulen</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>F. Meinhardt</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>R. Graul</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>M. Ramonet</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>W. Peters</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>E. J. Dlugokencky</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">European Commission Joint Research Centre, Ispra, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Marine and Atmospheric Research, Utrecht, Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Netherlands Energy Research Foundation (ECN), Petten, Netherlands</affiliation>
		<affiliation numeration="4" content_type="html">Umweltbundesamt, Messstelle Schauinsland, Kirchzarten, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Laboratoire des Sciences du Climat et de l’Environment (LSCE), Gif sur Yvette, France</affiliation>
		<affiliation numeration="6" content_type="html">NOAA Climate Monitoring and Diagnostics Laboratory, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A synthesis inversion based on the atmospheric zoom model TM5 is used to
derive top-down estimates of CH&lt;sub&gt;4&lt;/sub&gt; emissions from individual European
countries for the year 2001. We employ a model zoom over Europe with
1&amp;deg; &amp;times; 1&amp;deg; resolution that is two-way nested into the global model
domain (with resolution of 6&amp;deg; &amp;times; 4&amp;deg;. This approach ensures
consistent boundary conditions for the zoom domain and thus European
top-down estimates consistent with global CH&lt;sub&gt;4&lt;/sub&gt; observations. The TM5
model, driven by ECMWF analyses, simulates synoptic scale events at most
European and global sites fairly well, and the use of high-frequency
observations allows exploiting the information content of individual
synoptic events. A detailed source attribution is presented for a
comprehensive set of 56 monitoring sites, assigning the atmospheric signal
to the emissions of individual European countries and larger global regions.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
The available observational data put significant constraints on emissions
from different regions. Within Europe, in particular several Western
European countries are well constrained. The inversion results suggest up to
50-90% higher anthropogenic CH&lt;sub&gt;4&lt;/sub&gt; emissions in 2001 for Germany,
France and UK compared to reported UNFCCC values (EEA, 2003).
A recent revision of the German inventory, however, resulted in an increase
of reported CH&lt;sub&gt;4&lt;/sub&gt; emissions by 68.5% (EEA, 2004), being now in very
good agreement with our top-down estimate.
The top-down estimate for Finland is distinctly smaller than the a priori estimate,
suggesting much smaller CH&lt;sub&gt;4&lt;/sub&gt; emissions from Finnish wetlands than
derived from the bottom-up inventory.
The EU-15 totals are relatively close to UNFCCC values (within 4-30%) and
appear very robust for different inversion scenarios.</abstract>
	<references>
	</references>
</article>

