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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>16</volume_number>
		<volume_title>Observation, Prediction and Verification of Precipitation (EGU Session 2007)</volume_title>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/adgeo-16-131-2008</doi>
	<article_url>http://www.adv-geosci.net/16/131/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/16/131/2008/adgeo-16-131-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/16/131/2008/adgeo-16-131-2008.pdf</fulltext_pdf>
	<start_page>131</start_page>
	<end_page>136</end_page>
	<publication_date>2008-04-09</publication_date>
	<article_title content_type="html">The impact of an upper tropospheric teleconnection pattern on precipitation extremes over Cyprus</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Hatzaki</name>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>P. Lingis</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H.A. Flocas</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>S. Michaelides</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>C. Oikonomou</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Physics and Meteorology, Faculty of Physics, University of Athens, Greece</affiliation>
		<affiliation numeration="2" content_type="html">Meteorological Service of Cyprus, Cyprus</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Atmospheric Science, University of Edinburgh, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The objective of this study is to estimate the duration,
frequency and intensity of precipitation extreme episodes in Cyprus, in
relation with the two phases of the Eastern Mediterranean teleconnection
Pattern (EMP), during winter for the period 1958&amp;ndash;2005. A standardised
teleconnection index was employed to determine the phases (positive and
negative) and the strength of the EMP. The identification of the
precipitation extremes was performed with the aid of four climatic indices.
It was found that during the positive phase of the pattern, the length of
dry periods reduces while that of wet periods increases, being followed by
increase of frequency of extreme wet days and precipitation intensity. On
the contrary, during the negative phase, the dry spells become longer in
accordance with shortening of the wet spells, decrease of the number of
extreme wet days and precipitation intensity.</abstract>
	<references>
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</article>

