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	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>8</volume_number>
		<issue_number>20</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-6189-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/6189/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/6189/2008/acp-8-6189-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/6189/2008/acp-8-6189-2008.pdf</fulltext_pdf>
	<start_page>6189</start_page>
	<end_page>6197</end_page>
	<publication_date>2008-10-24</publication_date>
	<article_title content_type="html">Long-term observation of mass-independent oxygen isotope anomaly in stratospheric CO&lt;sub&gt;2&lt;/sub&gt;</article_title>
	<authors>
		<author numeration="1" affiliations="1,5">
			<name>S. Kawagucci</name>
			<email>kawagucci@ori.u-tokyo.ac.jp</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>U. Tsunogai</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S. Kudo</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>F. Nakagawa</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>H. Honda</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>S. Aoki</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>T. Nakazawa</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>M. Tsutsumi</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>T. Gamo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Earth and Planetary System Sciences, Faculty of Science, Hokkaido University, Sapporo, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Japan Aerospace Exploration Agency, Sagamihara, Japan</affiliation>
		<affiliation numeration="3" content_type="html">Center for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku University, Sendai, Japan</affiliation>
		<affiliation numeration="4" content_type="html">Dept. of Chemical Oceanography, Ocean Res. Ins., Univ. of Tokyo, Nakano-ku, Tokyo, Japan</affiliation>
		<affiliation numeration="5" content_type="html">present address: Dept. of Chemical Oceanography, Ocean Res. Ins., Univ. of Tokyo, Nakano-ku, Tokyo, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">Stratospheric and upper tropospheric air samples were collected during
1994â€“2004 over Sanriku, Japan and in 1997 over Kiruna, Sweden. Using these
archived air samples, we determined the triple oxygen-isotope composition of
stratospheric CO&lt;sub&gt;2&lt;/sub&gt; and the N&lt;sub&gt;2&lt;/sub&gt;O mixing ratio. The maximum &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;
value of +12.2&amp;permil;, resembling that observed previously in
the mesosphere at 60 km height, was found in the middle stratosphere over
Kiruna at 25.6 km height, suggesting that upper stratospheric and
mesospheric air descended to the middle stratosphere through strong downward
advection. A least-squares regression analysis of our observations on a
&amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;&amp;minus;&amp;delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; 
plot (&lt;i&gt;r&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&gt;0.95)
shows a slope of 1.63&amp;plusmn;pm0.10, which is similar to the reported value of
1.71&amp;plusmn;0.06, thereby confirming the linearity of three isotope
correlation with the slope of 1.6â€“1.7 in the mid-latitude lower and middle
stratosphere. The slope decrease with increasing altitude and a curvy trend
in three-isotope correlation reported from previous studies were not
statistically significant. Using negative linear correlations of &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;
and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; with the N&lt;sub&gt;2&lt;/sub&gt;O mixing
ratio, we quantified triple oxygen-isotope fluxes of CO&lt;sub&gt;2&lt;/sub&gt; to the
troposphere as +48&amp;permil; GtC/yr (&amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;) and +38&amp;permil; GtC/yr
(&amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;) with ~30% uncertainty. Comparing recent
model results and observations, underestimation of the three isotope slope
and the maximum &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt; value in the model were clarified,
suggesting a smaller O&lt;sub&gt;2&lt;/sub&gt; photolysis contribution than that of the model.
Simultaneous observations of &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;, &amp;delta;&lt;sup&gt;17&lt;/sup&gt;O&lt;sub&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;/sub&gt;, and N&lt;sub&gt;2&lt;/sub&gt;O mixing ratios can elucidate triple oxygen
isotopes in CO&lt;sub&gt;2&lt;/sub&gt; and clarify complex interactions among physical,
chemical, and photochemical processes occurring in the middle atmosphere.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alexander, B., Vollmer, M. K., Jackson, T., Weiss, R. F., and Thiemens, M. H.: Stratospheric CO&lt;sub&gt;2&lt;/sub&gt; isotopic anomalies and SF$_6$ and CFC tracer concentrations in the arctic polar vortex, Geophys. Res. Lett., 28, 4103â€“4106, 2001. </reference>
		<reference numeration="2" content_type="text"> Aoki, S., Nakazawa, T., Machida, T., Sugawara, S., Morimoto, S., Hashida, G., Yamanouchi, T., Kawamura, K., and Honda, H.: Carbon dioxide variations in the stratosphere over Japan, Scandinavia and Antarctica, Tellus B, 55, 178â€“186, 2003. </reference>
		<reference numeration="3" content_type="text"> Baertschi, P.: Absolute $^18$O content of standard mean ocean water, Earth Planet. Sc. Lett., 31, 341â€“344, 1976. </reference>
		<reference numeration="4" content_type="text"> Bhattacharya, S. K., Savarino, J., and Thiemens, M. H.: A new class of oxygen isotopic fractionation in photodissociation of carbon dioxide: Potential implications for atmospheres of Mars and Earth, Geophys. Res. Lett., 27, 1459â€“1462, 2000. </reference>
		<reference numeration="5" content_type="text"> Boering, K. A., Jackson, T., Hoag, K. J., Cole, A. S., Perri, M. J., Thiemens, M., and Atlas, E.: Observations of the anomalous oxygen isotopic composition of carbon dioxide in the lower stratosphere and the flux of the anomaly to the troposphere, Geophys. Res. Lett., 31, L03109, doi:10.1029/2003GL018451, 2004. </reference>
		<reference numeration="6" content_type="text"> Chakraborty, S. and Bhattacharya, S. K.: Experimental investigation of oxygen isotope exchange between CO&lt;sub&gt;2&lt;/sub&gt; and O($^1$D) and its relevance to the stratosphere, J. Geophys. Res.-Atmos., 108, 4724, doi:10.1029/2002JD002915, 2003. </reference>
		<reference numeration="7" content_type="text"> Ciais, P., Denning, A. S., Tans, P. P., Berry, J. A., Randall, D. A., Collatz, G. J., Sellers, P. J., White, J. W. C., Trolier, M., Meijer, H. A. J., Francey, R. J., Monfray, P., and Heimann, M.: A three-dimensional synthesis study of $\delta ^18$O in atmospheric CO&lt;sub&gt;2&lt;/sub&gt;: 1. Surface fluxes, J. Geophys. Res.-Atmos., 102, 5857â€“5872, 1997. </reference>
		<reference numeration="8" content_type="text"> Craig, H.: Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide, Geochim. Cosmochim. Acta, 12, 133â€“149, 1957. </reference>
		<reference numeration="9" content_type="text"> Cuntz, M., Ciais, P., Hoffmann, G., and Knorr, W.: A comprehensive global three-dimensional model of $\delta ^18$O in atmospheric CO&lt;sub&gt;2&lt;/sub&gt;: 1. Validation of surface processes, J. Geophys. Res.-Atmos., 108, 4528, doi:10.1029/2002JD003154, 2003. </reference>
		<reference numeration="10" content_type="text"> Gamo, T., Tsutsumi, M., Sakai, H., Nakazawa, T., Tanaka, M., Honda, H., Kubo, H., and Itoh, T.: Carbon and oxygen isotopic ratios of carbon dioxide a stratospheric profile over Japan, Tellus, 41B, 127â€“133, 1989. </reference>
		<reference numeration="11" content_type="text"> Gamo, T., Tsutsumi, M., Sakai, H., Nakazawa, T., Machida, T., Honda, H., and Itoh, T.: Long-term monitoring of carbon and oxygen-isotope ratios of stratospheric CO&lt;sub&gt;2&lt;/sub&gt; over Japan, Geophys. Res. Lett., 22, 397â€“400, 1995. </reference>
		<reference numeration="12" content_type="text"> Hoag, K. J., Still, C. J., Fung, I. Y., and Boering, K. A.: Triple oxygen isotope composition of tropospheric carbon dioxide as a tracer of terrestrial gross carbon fluxes, Geophys. Res. Lett., 32, L02802, doi:10.1029/2004GL021011, 2005. </reference>
		<reference numeration="13" content_type="text"> Honda, H., Aoki, S., Nakazawa, T., Morimoto, S., and Yajima, N.: Cryogenic air sampling system for measurements of the concentrations of stratospheric trace gases and their isotopic ratios over antarctica, J. Geomagn. Geoelectr., 48, 1145â€“1155, 1996. </reference>
		<reference numeration="14" content_type="text"> Honda, H.: Research on balloon-borne whole air sampling system for studying stratospheric minor constituents, Bulletin of Institute of Space and Astronautical Science , 115, 1â€“93, 2001 (in Japanese with English abstract). </reference>
		<reference numeration="15" content_type="text"> Kawagucci, S., Tsunogai, U., Kudo, S., Nakagawa, F., Honda, H., Aoki, S., Nakazawa, T., and Gamo, T.: An analytical system for determining $\delta ^17$O in CO&lt;sub&gt;2&lt;/sub&gt; using continuous flow-isotope ratio MS, Anal. Chem., 77, 4509â€“4514, 2005. </reference>
		<reference numeration="16" content_type="text"> Johnson, D. G., Jucks, K. W., Traub, W. A., and Chance, K. V.: Isotopic composition of stratospheric water vapor: Measurements and photochemistry, J. Geophys. Res.-Atmos., 106, 12 211â€“12 217, 2001. </reference>
		<reference numeration="17" content_type="text"> Johnston, J. C., RÃ¶ckmann, T., and Brenninkmeijer, C. A. M.: CO&lt;sub&gt;2&lt;/sub&gt; + O($^1$D) isotopic exchange: Laboratory and modeling studies, J. Geophys. Res., 105, 15 213â€“15 229, 2000. </reference>
		<reference numeration="18" content_type="text"> Lacoursiere, J., Meyer, S. A., Faris, G. W., Slanger, T. G., Lewis, B. R., and Gibson, S. T.: The O($^1$D) yield from O&lt;sub&gt;2&lt;/sub&gt; photodissociation near H Lyman-alpha (121.6 nm), J. Chem. Phys., 110, 1949â€“1958, 1999. </reference>
		<reference numeration="19" content_type="text"> LÃ¤mmerzahl, P., RÃ¶ckmann, T., Brenninkmeijer, C. A. M., Krankowsky, D., and Mauersberger, K.: Oxygen isotope composition of stratospheric carbon dioxide, Geophys. Res. Lett., 29, 1582, doi:10.1029/2001GL014343, 2002. </reference>
		<reference numeration="20" content_type="text"> Liang, M. C., Blake, G. A., Lewis, B. R., and Yung, Y. L.: Oxygen isotopic composition of carbon dioxide in the middle atmosphere, Proceedings of the National Academy of Sciences of the United States of America, 104, 21â€“25, 2007. </reference>
		<reference numeration="21" content_type="text"> Matsuhisa, Y., Goldsmith, J. R., and Clayton, R. N.: Mechanism of hydrothermal crystallization of quartz at 250&amp;deg;C and 15 kbar, Geochim. Cosmochim. Acta, 42, 173â€“182, 1978. </reference>
		<reference numeration="22" content_type="text"> Mauersberger, K.: Ozone isotope measurements in the stratosphere, Geophys. Res. Lett., 14, 80â€“83, 1987. </reference>
		<reference numeration="23" content_type="text"> Miller, M. F.: Isotopic fractionation and the quantification of $^17$O anomalies in the oxygen three-isotope system: An appraisal and geochemical significance, Geochim. Cosmochim. Acta, 66, 1881â€“1889, 2002. </reference>
		<reference numeration="24" content_type="text"> Miller, M. F., RÃ¶ckmann, T., and Wright, I. P.: A general algorithm for the $^17$O abundance correction to $^13$C/$^12$C determinations from CO&lt;sub&gt;2&lt;/sub&gt; isotopologue measurements, including CO&lt;sub&gt;2&lt;/sub&gt; characterised by `mass-independent&apos; oxygen isotope distributions, Geochim. Cosmochim. Acta, 71, 3145â€“3161, 2007. </reference>
		<reference numeration="25" content_type="text"> Nakazawa, T., Machida, T., Sugawara, S., Murayama, S., Morimoto, S., and Hashida, G.: Measurements of the stratospheric carbon-dioxide concentration over Japan using a balloon-borne cryogenic sampler, Geophys. Res. Lett., 22, 1229â€“1232, 1995. </reference>
		<reference numeration="26" content_type="text"> Perri, M. J., Van Wyngarden, A. L., Boering, K. A., Lin, J. J., and Lee, Y. T.: Dynamics of the O($^1$D)+CO&lt;sub&gt;2&lt;/sub&gt; oxygen isotope exchange reaction, J. Chem. Phys., 119, 8213â€“8216, 2003. </reference>
		<reference numeration="27" content_type="text"> Plumb, R. A. and Ko, M. K. W.: Interrelationships between mixing ratios of long lived stratospheric constituents, J. Geophys. Res.-Atmos., 97, 10 145â€“10 156, 1992. </reference>
		<reference numeration="28" content_type="text"> Prather, M. J. and Ehhalt, D.: 3rd report of the Intergovernmental Panel on Climate Change, in: Climate Change, edited by: Houghton, J., et al., Cambridge Univ. Press, New York, 239â€“287, 2001. </reference>
		<reference numeration="29" content_type="text"> Santrock, J., Studley, S. A., and Hayes, J. M.: Isotopic analyses based on the mass spectrum of carbon dioxide, Anal. Chem., 57, 1444â€“1448, 1985. </reference>
		<reference numeration="30" content_type="text"> Shaheen, R., Janssen, C., and Röckmann, T.: Investigations of the photochemical isotope equilibrium between O&lt;sub&gt;2&lt;/sub&gt;, CO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt;, Atmos. Chem. Phys., 7, 495â€“509, 2007. </reference>
		<reference numeration="31" content_type="text"> Thiemens, M. H. and Heidenreich, J. E.: The mass-independent fractionation of oxygen â€“ a novel isotope effect and its possible cosmochemical implications, Science, 219, 1073â€“1075, 1983. </reference>
		<reference numeration="32" content_type="text"> Thiemens, M. H., Jackson, T., Mauersberger, K., Schueler, B., and Morton, J.: Oxygen isotope fractionation in stratospheric CO&lt;sub&gt;2&lt;/sub&gt;, Geophys. Res. Lett., 18, 669â€“672, 1991. </reference>
		<reference numeration="33" content_type="text"> Thiemens, M. H., Jackson, T. L., and Brenninkmeijer, C. A. M.: Observation of a mass-independent oxygen isotopic composition in terrestrial stratospheric CO&lt;sub&gt;2&lt;/sub&gt;, the link to ozone chemistry, and the possible occurrence in the Martian atmosphere, Geophys. Res. Lett., 22, 255â€“257, 1995a. </reference>
		<reference numeration="34" content_type="text"> Thiemens, M. H., Jackson, T., Zipf, E. C., Erdman, P. W., and van Egmond, C.: Carbon-dioxide and oxygen-isotope anomalies in the mesosphere and stratosphere, Science, 270, 969â€“972, 1995b. </reference>
		<reference numeration="35" content_type="text"> Thiemens, M. H.: Mass-independent isotope effects in planetary atmospheres and the early solar system, Science, 283, 341â€“345, 1999. </reference>
		<reference numeration="36" content_type="text"> Waugh, D. W. and Hall, T. M.: Age of stratospheric air: Theory, observations, and models, Rev. Geophys., 40, 1010, doi:10.1029/2000RG000101, 2002. </reference>
		<reference numeration="37" content_type="text"> Wen, J. and M. H. Thiemens, Multi-isotope study of the O($^1$D) + CO&lt;sub&gt;2&lt;/sub&gt; exchange and stratospheric consequences, J. Geophys. Res., 98, 12 801â€“12 808, 1993. </reference>
		<reference numeration="38" content_type="text"> Young, E. D., Galy, A., and Nagahara, H.: Kinetic and equilibrium mass-dependent isotope fractionation laws in nature and their geochemical and cosmochemical significance, Geochim. Cosmochim. Acta, 66, 1095â€“1104, 2002. </reference>
		<reference numeration="39" content_type="text"> Yung, Y. L., Demore, W. B., and Pinto, J. P.: Isotopic exchange between carbon dioxide and ozone via O($^1$D) in the stratosphere, Geophys. Res. Lett., 18, 13â€“16, 1991. </reference>
	</references>
</article>

