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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-817-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/817/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/817/2009/cpd-5-817-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/817/2009/cpd-5-817-2009.pdf</fulltext_pdf>
	<start_page>817</start_page>
	<end_page>851</end_page>
	<publication_date>2009-03-04</publication_date>
	<article_title content_type="html">Uncertainties in modeling CH&lt;sub&gt;4&lt;/sub&gt; emissions from northern wetlands in glacial climates: effect of hydrological model and CH&lt;sub&gt;4&lt;/sub&gt; model structure</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Berrittella</name>
			<email>cberri@falw.vu.nl</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. van Huissteden</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Vrije Universiteit, Faculty of Earth and Life Sciences, Department of Hydrology and Geo-Environmental Sciences, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">Methane (CH&lt;sub&gt;4&lt;/sub&gt;) fluxes from northern wetlands may have influenced
atmospheric CH&lt;sub&gt;4&lt;/sub&gt; concentrations at climate warming phases during the
800 000 years and at present global warming. Including these CH&lt;sub&gt;4&lt;/sub&gt; fluxes
in earth system models is essential to understand feedbacks between climate
and atmospheric composition.

&lt;br&gt;&lt;br&gt;

Attempts to model CH&lt;sub&gt;4&lt;/sub&gt; fluxes from wetlands have been undertaken
previously using various approaches. Here, we test a process-based wetland
CH&lt;sub&gt;4&lt;/sub&gt; flux model (PEATLAND-VU) which includes details of soil-atmosphere
CH&lt;sub&gt;4&lt;/sub&gt; transport. The model has been used to simulate CH&lt;sub&gt;4&lt;/sub&gt; emissions
from continental Europe in different glacial climates and the present
climate.

&lt;br&gt;&lt;br&gt;

This paper displays results on the sensitivity of modeling glacial
terrestrial CH&lt;sub&gt;4&lt;/sub&gt; fluxes to basic tuning parameters of the model, to
different approaches in modeling of the water table, and to model structure.
For testing the model structure, PEATLAND-VU has been compared to a simpler
modeling approach based on wetland primary production estimated from a
vegetation model (BIOME). The tuning parameters are the CH&lt;sub&gt;4&lt;/sub&gt; production
rate from labile organic carbon and its temperature sensitivity.

&lt;br&gt;&lt;br&gt;

The modelled fluxes prove comparatively insensitive to hydrology
representation, and sensitive to microbial parameters and model structure.
Glacial climate emissions are also highly sensitive to assumptions on the
extent of ice cover and exposed seafloors. Wetland expansion on low relief
exposed seafloor areas, may have compensated for a decrease of wetland area
due to continental ice cover.</abstract>
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