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<article language="en">
	<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>7</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-1925-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/1925/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/1925/2008/acp-8-1925-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/1925/2008/acp-8-1925-2008.pdf</fulltext_pdf>
	<start_page>1925</start_page>
	<end_page>1935</end_page>
	<publication_date>2008-04-03</publication_date>
	<article_title content_type="html">Normal mode Rossby waves and their effects on chemical composition in the late summer stratosphere</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Pendlebury</name>
			<email>diane@atmosp.physics.utoronto.ca</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. G. Shepherd</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>M. Pritchard</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>C. McLandress</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Toronto, Toronto, Canada</affiliation>
		<affiliation numeration="2" content_type="html">now at: University of California, San Diego, USA</affiliation>
	</affiliations>
	<abstract content_type="html">During past MANTRA campaigns, ground-based measurements of several long-lived chemical species
have revealed quasi-periodic fluctuations on time scales of several days.  These fluctuations could
 confound efforts to detect long-term trends from MANTRA, and need to be understood and accounted
for. Using the Canadian Middle Atmosphere Model, we investigate
the role of dynamical variability in the late summer stratosphere due to normal mode Rossby waves
and the impact of this variability on fluctuations in chemical species.
Zonal wavenumber 1, westward travelling waves are considered with average periods of 5, 10 and
16 days. Time-lagged correlations between the temperature and nitrous oxide, methane and
ozone fields are calculated in order to assess the possible impact of these waves on
the chemical species.
Using Fourier-wavelet decomposition and correlating the fluctuations between the temperature and
chemical fields, we determine that variations in the chemical species are well-correlated
with the 5- and 10-day waves between 30 and 60 km, although the nature of the correlations depend
strongly on altitude. Interannual variability of the waves is also examined.</abstract>
	<references>
		<reference numeration="1" content_type="text"> %</reference>
		<reference numeration="2" content_type="text"> %</reference>
		<reference numeration="3" content_type="text"> %</reference>
		<reference numeration="4" content_type="text"> %\beginthebibliography </reference>
		<reference numeration="5" content_type="text"> Austin, J., Shindell, D., Brühl, C., Dameris, M., Manzini, E., Nagashima, T., Newman, P., Pawson, S., Pitari, G., Rozanov, E., C Schnadt, C., and Shepherd, T G.: Uncertainties and assessments of chemistry-climate models of the stratosphere, Atmos. Chem. Phys., 3, 1&amp;ndash;27, 2003. </reference>
		<reference numeration="6" content_type="text"> Beagley, S R., de~Grandprè, J., Koshyk, J N., McFarlane, N A., and Shepherd, T G.: Radiative-dynamical climatology of the first-generation Canadian Middle Atmosphere Model, Atmos.-Ocean, 35, 293&amp;ndash;331, 1997. </reference>
		<reference numeration="7" content_type="text"> Cheong, H.-B. and Kimura, R.: Excitation of the 5-day wave by Antarctica, J. Atmos. Sci., 54, 87&amp;ndash;102, 1997. </reference>
		<reference numeration="8" content_type="text"> Cheong, H.-B. and Kimura, R.: Excitation of the 10-day and 14-day waves, J. Atmos. Sci., 58, 1129&amp;ndash;1145, 2001. </reference>
		<reference numeration="9" content_type="text"> de~Grandprè, J., Beagley, S R., Fomichev, V I., Griffioen, E., McConnell, J C., Medvedev, A S., and Shepherd, T G.: Ozone climatology using interactive chemistry: Results from the Canadian Middle Atmosphere Model, J. Geophys. Res., 105, 26 475&amp;ndash;26 491, 2000. </reference>
		<reference numeration="10" content_type="text"> Geisler, J E. and Dickinson, R E.: The five-day wave on a sphere with realistic zonal winds, J. Atmos. Sci., 33, 632&amp;ndash;641, 1976. </reference>
		<reference numeration="11" content_type="text"> Hines, C O.: Doppler-spread parameterization of gravity-wave momentum deposition in the middle atmosphere. Part 1: Basic formulation, J. Atmos. and Solar-Terr. Phys., 59, 371&amp;ndash;386, 1997. </reference>
		<reference numeration="12" content_type="text"> Hirooka, T.: Normal mode Rossby waves as revealed by UARS/IASMS observations, J. Atmos. Sci., 57, 1277&amp;ndash;1285, 2000. </reference>
		<reference numeration="13" content_type="text"> Hirooka, T. and Hirota, I.: Further evidence of normal mode Rossby waves, Pageoph., 130, 277&amp;ndash;289, 1989. </reference>
		<reference numeration="14" content_type="text"> Hirota, I. and Hirooka, T.: Normal mode Rossby waves observed in the upper stratosphere. Part I: First symmetric modes of zonal wavenumbers 1 and 2, J. Atmos. Sci., 41, 1253&amp;ndash;1267, 1983. </reference>
		<reference numeration="15" content_type="text">Madden, R. A.: Further Evidence of Traveling Planetary Waves, J. Atmos. Sci., 35, 1605&amp;ndash;1618, 1978. </reference>
		<reference numeration="16" content_type="text"> Madden, R. and Julian, P.: Further evidence of global-scale, 5-day pressure waves, J. Atmos. Sci., 29, 1464&amp;ndash;1469, 1972. </reference>
		<reference numeration="17" content_type="text"> McLandress, C.: Seasonal variability of the diurnal tide: Results from the Canadian middle atmosphere general circulation model, J. Geophys. Res., 102, 29,747&amp;ndash;29,764, 1997. </reference>
		<reference numeration="18" content_type="text"> McLandress, C.: On the importance of gravity waves in the middle atmosphere and their parameterization in general circulation models, J. Atmos. Sol.- Terr. Phys., 60, 1357&amp;ndash;1383, 1998. </reference>
		<reference numeration="19" content_type="text"> Miyoshi, Y.: Numerical simulation of the 5-day and 16-day waves in the mesopause region, Earth Planets Space, 51, 763&amp;ndash;772, 1999. </reference>
		<reference numeration="20" content_type="text"> Miyoshi, Y. and Hirooka, T.: A numerical experiment of excitation of the 5-day wave by a GCM, J. Atmos. Sci., 56, 1698&amp;ndash;1707, 1999. </reference>
		<reference numeration="21" content_type="text"> Prata, A J.: Observations of the 5-day wave in the stratosphere and mesosphere, J. Atmos. Sci., 46, 2473&amp;ndash;2477, 1989. </reference>
		<reference numeration="22" content_type="text"> Salby, M L.: Rossby normal modes in nonuniform background configurations. Part II: Equinox and solstice conditions, J. Atmos. Sci., 38, 1827&amp;ndash;1840, 1981. </reference>
		<reference numeration="23" content_type="text"> Sankey, D. and Shepherd, T G.: Correlations of long-lived chemical species in a middle atmosphere general circulation model, J. Geophys. Res., 108, 10.1029/2002JD002 799, 2003. </reference>
		<reference numeration="24" content_type="text"> Sciremammano, F., Jr.: A suggestion for the presentation of correlations and their significance levels, J. Phys. Ocean., 9, 1273&amp;ndash;1276, 1979. </reference>
	</references>
</article>

