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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>25</volume_number>
		<volume_title>Precipitation: Measurement, Climatology, Remote Sensing, and Modeling (EGU Session 2009)</volume_title>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/adgeo-25-45-2010</doi>
	<article_url>http://www.adv-geosci.net/25/45/2010/</article_url>
	<abstract_html>http://www.adv-geosci.net/25/45/2010/adgeo-25-45-2010.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/25/45/2010/adgeo-25-45-2010.pdf</fulltext_pdf>
	<start_page>45</start_page>
	<end_page>50</end_page>
	<publication_date>2010-03-09</publication_date>
	<article_title content_type="html">Cyclic modes of the intra-annual variability of precipitation in Greece</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. T. Nastos</name>
			<email>nastos@geol.uoa.gr</email>
		</author>
		<author numeration="2" affiliations="1,2,3">
			<name>C. S. Zerefos</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory of Climatology and Atmospheric Environment, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece</affiliation>
		<affiliation numeration="2" content_type="html">National Observatory of Athens, Athens, Greece</affiliation>
		<affiliation numeration="3" content_type="html">Research Center for Atmospheric Physics and Climatology of the Academy of Athens, Athens, Greece</affiliation>
	</affiliations>
	<abstract content_type="html">The application of harmonic analysis to the annual
variability of precipitation is the object of this study, so that the modes,
which compose the annual variability, be elicited. For this purpose, monthly
precipitation totals from 30 meteorological stations of the Hellenic
National Meteorological Service (HNMS), for the period 1950–2000, were used.
&lt;br&gt;&lt;br&gt;
The initial target is to reduce the number of variables and to detect
structure in the relationships between the variables. The most commonly used
technique for this purpose is the application of Factor Analysis (FA)
resulted in five main factors (sub-regions) with common precipitation
characteristics, explaining 77% of the total variance. For each
sub-region, a representative station is selected for the analyses, mainly,
as the station within the sub-region with the highest factor loading. In the
process, the Fourier Analysis is applied to the mean monthly precipitation,
so that 2 harmonic components are derived, which explain more than 90% of
the total variability of each station, and are due to different synoptic and
thermodynamic processes associated with Greece&apos;s precipitation regime.
Finally the calculation of the time of the maximum precipitation, for each
harmonic component, gives the spatial distribution of the appearance of the
maximum precipitation in the Greek region.</abstract>
	<references>
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</article>

