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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-137-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/137/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/137/2008/acpd-8-137-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/137/2008/acpd-8-137-2008.pdf</fulltext_pdf>
	<start_page>137</start_page>
	<end_page>160</end_page>
	<publication_date>2008-01-08</publication_date>
	<article_title content_type="html">Sensitivity of tracer transport to model resolution, forcing data and tracer lifetime in the general circulation model ECHAM5</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Aghedo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Rast</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. G. Schultz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Meteorology, Hamburg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">ICG-2, Research Centre, Jülich, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The transport of tracers in the general circulation model ECHAM5 is
analysed using 9 independent idealized tracers with constant lifetimes
released in different altitude regions of the atmosphere. The source
regions were split into the tropics, Northern and Southern
Hemisphere. The dependency of tracer transport on model resolution is
tested in the resolutions T21L19, T42L19, T42L31, T63L31 and T106L31,
by employing tracers with a globally uniform lifetime of 5
months. Each of the experiments uses prescribed sea surface
temperatures and sea ice fields of the 1990s.  The influence of
meteorology and tracer lifetimes were tested by performing
additional experiments in the T63L31 resolution, by nudging ECHAM5 towards the European
Centre for Medium Range Weather Forecast 40 years re-analysis data
(ERA40), and by using tracer lifetimes of 0.5 and 50 months,
respectively.  The transport of tracers is faster in the finer
resolution models and is mostly dependent on the number of vertical
levels. We found a decrease in the inter-hemispheric transport of
tracers with source region at the surface or the tropopause in the
coarse resolution models due to increasing recirculation within the
source region and vertical mixing. However, a coarse model resolution
leads to enhanced inter-hemispheric transport in the stratosphere. The
use of ERA40 data only slightly affects the inter-hemispheric
transport of surface and tropopause tracers, whereas it increases the
inter-hemispheric and vertical transport in the stratosphere by up to
100% and by a factor of 2.5, respectively. The inter-hemispheric
transport time was deduced from simulations with tracers of infinite lifetime and source regions at the surface
in the Northern and Southern Hemisphere. Again, the transport was
found to be faster for models with higher vertical resolution. We
find inter-hemispheric transport times of about 7 to 9 months which
are lower than the values reported in the literature, based for example on &lt;sup&gt;85&lt;/sup&gt;Kr observations.</abstract>
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</article>

