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	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>15</volume_number>
		<volume_title>Topics in modern geophysical fluid dynamics</volume_title>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/adgeo-15-23-2008</doi>
	<article_url>http://www.adv-geosci.net/15/23/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/15/23/2008/adgeo-15-23-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/15/23/2008/adgeo-15-23-2008.pdf</fulltext_pdf>
	<start_page>23</start_page>
	<end_page>33</end_page>
	<publication_date>2008-03-18</publication_date>
	<article_title content_type="html">An unified approach to meteorological modelling based on multiple-scales asymptotics</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Klein</name>
			<email>rupert.klein@zib.de</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">FB Mathematik &amp; Informatik, Freie Universität Berlin, Arnimallee 2&amp;ndash;6, 14195 Berlin, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">In 2003, the author suggested a mathematical framework for the derivation of reduced
meteorological models at a Mathematics conference (5th ICIAM, Sydney, Australia),
(Klein, 2004). The framework consists of (i) non-dimensionalization of the 3-D compressible
flow equations on the rotating sphere, (ii) identification of universal non-dimensional
parameters, (iii) distinguished limits between these and additional problem-specific
parameters, and (iv) multiple scales expansions in the remaining small parameter
&amp;epsilon;.
This parameter may be interpreted as the cubic root of the centripetal acceleration due
to the Earth&apos;s rotation divided by the acceleration of gravity, see also Keller (1951), Eq. (10).
For the mojority of reduced models of theoretical meteorology that we have come across,
the approach allowed us to generate systematic derivations starting directly from the 3-D
compressible flow equations on the rotating sphere. The framework&apos;s potential fully
shows in multiscale interaction studies such as Klein (2006), in which we incorporated bulk
microphysics closures for moist processes and derived scale interaction models for
deep convection. Currently, we study the structure, evolution, and motion of Hurricane
strength H1/H2 vortices (Mikusky, 2007), large-scale stratocumulus cloud decks, and planetary-synoptic
scale interaction models which should be relevant for Earth System Models
of Intermediate Complexity (EMICs). Here we summarize the general framework and use
the example of quasi-geostrophic theory to demonstrate its application.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Biello, J. and Majda, A.: Transformations for temperature flux in multiscale models of the tropics, Theor. Comp. Fluid Dyn., 20, 405&amp;ndash;420, 2006. </reference>
		<reference numeration="2" content_type="text"> Botta, N., Klein, R., and Almgren, A.: Dry atmosphere asymptotics, PIK-Report 55, Potsdam Institute for Climate Impact Research, 1999. </reference>
		<reference numeration="3" content_type="text"> Botta, N., Klein, R., and Almgren, A.: Asymptotic Analysis of a Dry Atmosphere, in: ENUMATH 99 - Proc. 3rd Europ. Conf. on Num. Math., Jyväskylä, Finland, edited by: Neittaanmäki, P. and Tiihonen, T., World Scientific, Singapore, 2000. </reference>
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		<reference numeration="6" content_type="text"> Keller, J. and Ting, L.: Approximate equations for large scale atmospheric motions, Internal Report, Inst. for Mathematics &amp; Mechanics (renamed to Courant Institute of Mathematical Sciences in 1962), NYU, (http://www.arxiv.org/abs/physics/0606114), 1951. </reference>
		<reference numeration="7" content_type="text"> Klein, R.: Asymptotic Analyses for Atmospheric Flows and the Construction of Asymptotically Adaptive Numerical Methods, ZAMM, 80, 765&amp;ndash;777, 2000. </reference>
		<reference numeration="8" content_type="text"> Klein, R.: An applied mathematical view of meteorological modelling, in: Applied Mathematics Entering the 21st century, Invited talks from the ICIAM 2003 Congress, Vol. 116, SIAM Proceedings in Applied Mathematics, 177&amp;ndash;219, 2004. </reference>
		<reference numeration="9" content_type="text"> Klein, R. and Majda, A.: Systematic multiscale models for deep convection on mesoscales, Theor. Comp. Fluid Dyn., 20, 525&amp;ndash;551, 2006. </reference>
		<reference numeration="10" content_type="text"> Klein, R., Mikusky, E., and Owinoh, A.: Multiple scales asymptotics for atmospheric flows, in: 4th European Conference of Mathematics, Stockholm, Sweden, edited by: Laptev, A., European Mathematical Society Publishing House, 201&amp;ndash;220, 2004. </reference>
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</article>

