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<article language="en">
	<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>17</volume_number>
		<volume_title>9th EGU Plinius Conference on Mediterranean Storms (2007)</volume_title>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/adgeo-17-1-2008</doi>
	<article_url>http://www.adv-geosci.net/17/1/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/17/1/2008/adgeo-17-1-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/17/1/2008/adgeo-17-1-2008.pdf</fulltext_pdf>
	<start_page>1</start_page>
	<end_page>4</end_page>
	<publication_date>2008-06-20</publication_date>
	<article_title content_type="html">Numerical study of two-dimensional moist symmetric instability</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Fantini</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. Malguzzi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">ISAC-CNR, via Gobetti 101, 40129 Bologna, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">The 2-D version of the non-hydrostatic fully compressible model MOLOCH
developed at ISAC-CNR was used in idealized set-up to study the start-up
and finite amplitude evolution of symmetric instability. The unstable
basic state was designed by numerical integration of the equation
which defines saturated equivalent potential vorticity q&lt;sub&gt;e&lt;/sub&gt;&lt;sup&gt;*&lt;/sup&gt;.
We present the structure and growth rates of the linear modes
both for a supersaturated initial state (&quot;super&quot;-linear mode) and
for a saturated one (&quot;pseudo&quot;-linear mode) and the
modifications induced on the base state by their
finite amplitude evolution.</abstract>
	<references>
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</article>

