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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>4</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-1817-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/1817/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/1817/2004/acpd-4-1817-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/1817/2004/acpd-4-1817-2004.pdf</fulltext_pdf>
	<start_page>1817</start_page>
	<end_page>1853</end_page>
	<publication_date>2004-03-24</publication_date>
	<article_title content_type="html">Model calculations of the age of firn air across the Antarctic continent</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. A. Kaspers</name>
			<email>k.a.kaspers@phys.uu.nl</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. S. W. van de Wal</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. R. van de Broeke</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>J. Schwander</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>N. P. M. van Lipzig</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>C. A. M. Brenninkmeijer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, 3584 CC Utrecht, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">Physics Institute, University of Bern, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">British Antarctic Survey, Cambridge, United Kingdom</affiliation>
		<affiliation numeration="4" content_type="html">Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The age of firn air in Antarctica at pore close-off depth is only known for
a few specific sites where firn air has been sampled for analyses. We
present a model that calculates the age of firn air at pore close-off depth
for the entire Antarctic continent. The model basically uses four
meteorological parameters as input (surface temperature, pressure,
accumulation rate and wind speed). Using parameterisations for surface snow
density, pore close-off density and tortuosity, in combination with a
density-depth model and data of a regional atmospheric climate model,
distribution of pore close-off depth for the entire Antarctic continent is
determined. The deepest pore close-off depth was found for the East
Antarctic Plateau near 72&amp;deg; E, 82&amp;deg; S, at 150&amp;plusmn;15 m
(2&amp;sigma;). A firn air diffusion model was applied to calculate the age of
CO&lt;sub&gt;2&lt;/sub&gt; at pore close-off depth. The results predict that the oldest firn
gas (CO&lt;sub&gt;2&lt;/sub&gt; age) is located between Dome Fuji, Dome Argos and Vostok at
43&amp;deg; E, 78&amp;deg; S being 148&amp;plusmn;23 (1&amp;sigma; or 38 for
2&amp;sigma;) years old. At this location an atmospheric trace gas record
should be obtained. In this study we show that methyl chloride could be
recorded with a predicted length of 125 years as an example for trace gas
records at this location. The longest record currently available from firn
air is derived at South Pole, being 80 years.

&lt;br&gt;&lt;br&gt;
Sensitivity tests reveal that the locations with old firn air (East
Antarctic Plateau) have an estimated uncertainty (2&amp;sigma;) for the
modelled CO&lt;sub&gt;2&lt;/sub&gt; age at pore close-off depth of 30% and of about 40%
for locations with younger firn air (CO&lt;sub&gt;2&lt;/sub&gt; age typically 40 years).
Comparing the modelled age of CO&lt;sub&gt;2&lt;/sub&gt; at pore close-off depth with directly
determined ages at seven sites yielded a correlation coefficient of 0.90 and
a slope close to 1, suggesting a high level of confidence for the modelled
results in spite of considerable remaining uncertainties.</abstract>
	<references>
	</references>
</article>

