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<article language="en">
	<journal>
		<journal_title>Geoscientific Model Development Discussions</journal_title>
		<journal_url>www.geosci-model-dev-discuss.net</journal_url>
		<issn>1991-9611</issn>
		<eissn>1991-962X</eissn>
		<volume_number>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/gmdd-1-147-2008</doi>
	<article_url>http://www.geosci-model-dev-discuss.net/1/147/2008/</article_url>
	<abstract_html>http://www.geosci-model-dev-discuss.net/1/147/2008/gmdd-1-147-2008.html</abstract_html>
	<fulltext_pdf>http://www.geosci-model-dev-discuss.net/1/147/2008/gmdd-1-147-2008.pdf</fulltext_pdf>
	<start_page>147</start_page>
	<end_page>185</end_page>
	<publication_date>2008-07-28</publication_date>
	<article_title content_type="html">A description of the FAMOUS (version XDBUA) climate model and control run</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. S. Smith</name>
			<email>r.s.smith@reading.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>J. M. Gregory</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. Osprey</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NCAS-Climate, Walker Institute, Reading, UK</affiliation>
		<affiliation numeration="2" content_type="html">Met Office Hadley Centre, Exeter, UK</affiliation>
	</affiliations>
	<abstract content_type="html">FAMOUS is an ocean-atmosphere general circulation model of low resolution,
capable of simulating well in excess of 100 years of model climate per
wallclock day using current high performance computing facilities. It uses
most of the same code as HadCM3, a widely used climate model of higher
resolution and computational cost, and has been tuned to reproduce the same
climate reasonably well. FAMOUS is useful for climate simulations where the
computational cost makes the application of HadCM3 unfeasible, either because
of the length of simulation or the size of the ensemble desired. We document
a number of scientific and technical improvements to the original version of
FAMOUS. These improvements include changes to the parameterisations of ozone
and sea-ice which remove a significant cold bias from high northern latitudes
and the upper troposphere, and the elimination of volume-averaged drifts in
ocean tracers. There are also changes to the model infrastructure which
facilitate paleoclimate simulations.</abstract>
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