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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>10</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-1631-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/1631/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/1631/2010/acpd-10-1631-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/1631/2010/acpd-10-1631-2010.pdf</fulltext_pdf>
	<start_page>1631</start_page>
	<end_page>1657</end_page>
	<publication_date>2010-01-21</publication_date>
	<article_title content_type="html">Post-coring entrapment of modern air in polar ice cores collected near  the firn-ice transition: evidence from CFC-12 measurements in Antarctic firn air and shallow ice cores</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Aydin</name>
			<email>maydin@uci.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. A. Montzka</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>M. O. Battle</name>
		</author>
		<author numeration="4" affiliations="6">
			<name>M. B. Williams</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>W. De Bruyn</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>J. H. Butler</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>K. R. Verhulst</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>C. Tatum</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>B. K. Gun</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>D. A. Plotkin</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>B. D. Hall</name>
		</author>
		<author numeration="12" affiliations="1">
			<name>E. S. Saltzman</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth System Science, University of California, Irvine, California, USA</affiliation>
		<affiliation numeration="2" content_type="html">Earth System Research Laboratories – Global Monitoring Division, National Oceanic and Atmospheric Administration, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Physics and Astronomy, Bowdoin College, Brunswick, Maine, USA</affiliation>
		<affiliation numeration="4" content_type="html">Schmid College of Science, Chapman University, Orange, California, USA</affiliation>
		<affiliation numeration="5" content_type="html">Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA</affiliation>
		<affiliation numeration="6" content_type="html">ICF International, San Francisco, California, USA</affiliation>
	</affiliations>
	<abstract content_type="html">In this study, we report the first measurements of CFC-12
      (CCl&lt;sub&gt;2&lt;/sub&gt;F&lt;sub&gt;2&lt;/sub&gt;) in air extracted from shallow ice cores along with
      firn air CFC-12 measurements from three Antarctic sites. The firn air
      data are consistent with the known atmospheric history of CFC-12. In
      contrast, the ice core samples collected near the firn-ice transition
      exhibit anomalously high CFC-12 levels. Together, the ice core and
      firn air data provide evidence for presence of modern air entrapped in
      shallow ice core samples. We propose that this is due to closure of
      open pores after drilling, entrapping modern air and resulting in
      elevated CFC-12 mixing ratios. Our measurements reveal the presence of
      open porosity below the depth at which firn air samples can be
      collected and demonstrate how the composition of bubble air in shallow
      ice cores can be altered during the post-drilling period through
      purely physical processes. These results have implications for
      investigations involving trace gas composition of bubbles in shallow
      ice cores.</abstract>
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</article>

