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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-17-87-2008</doi>
	<article_url>http://www.adv-geosci.net/17/87/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/17/87/2008/adgeo-17-87-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/17/87/2008/adgeo-17-87-2008.pdf</fulltext_pdf>
	<start_page>87</start_page>
	<end_page>91</end_page>
	<publication_date>2008-12-22</publication_date>
	<article_title content_type="html">Precipitation climatology over Mediterranean Basin from ten years of TRMM measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. V. Mehta</name>
			<email>amita@radar.gsfc.nasa.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. Yang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD 21228, USA</affiliation>
		<affiliation numeration="2" content_type="html">I. M. Systems Group and Center for Satellite Applications and Research (STAR)/NESDIS/ NOAA, Camp Springs, MD 20746, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Climatological features of mesoscale rain activities over the Mediterranean
region between 5&amp;deg; W–40&amp;deg; E and 28&amp;deg; N–48&amp;deg; N are examined
using the Tropical Rainfall Measuring Mission (TRMM) 3B42 and 2A25 rain
products. The 3B42 rainrates at 3-hourly, 0.25&amp;deg;&amp;times;0.25&amp;deg; spatial
resolution for the last 10 years (January 1998 to July 2007) are used to
form and analyze the 5-day mean and monthly mean climatology of rainfall.
Results show considerable regional and seasonal differences of rainfall over
the Mediterranean Region. The maximum rainfall (3–5 mm day&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) occurs
over the mountain regions of Europe, while the minimum rainfall is observed
over North Africa (~0.5 mm day&lt;sup&gt;&amp;minus;1&lt;/sup&gt;). The main rainy season over
the Mediterranean Sea extends from October to March, with maximum rainfall
occurring during November–December. Over the Mediterranean Sea, an average
rainrate of ~1–2 mm day&lt;sup&gt;&amp;minus;1&lt;/sup&gt; is observed, but during the rainy
season there is 20% larger rainfall over the western Mediterranean Sea
than that over the eastern Mediterranean Sea. During the rainy season,
mesoscale rain systems generally propagate from west to east and from north
to south over the Mediterranean region, likely to be associated with
Mediterranean cyclonic disturbances resulting from interactions among
large-scale circulation, orography, and land-sea temperature contrast.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alpert, P., Baldi, M., Ilani, R., et al.: Relations between climate variability in the Mediterranean region and the tropics: ENSO, South Asian and African monsoons, hurricanes and Saharan dust, Mediterranean Climate Variability, Elsevier B. V., 149–177, 2006. </reference>
		<reference numeration="2" content_type="text"> Homar, V., Jansa, A., Campins, J., Genoves, A., and Ramis. C.: Towards a systematic climatology of sensitivities of Mediterranean high impact weather: a contribution based on intense cyclones, Nat. Hazards Earth Syst. Sci., 7, 445–454, 2007. </reference>
		<reference numeration="3" content_type="text"> Huffman, G. J., Adler, R. F., Bolvin, D. T., Gu, G., Nelkin, E. J., Bowman, K. P., Hong, Y., Stocker, E. F., and Wolff, D. B.: The TRMM Multi-satellite Precipitation Analysis (TMPA): quasi-global, multi-year, combined-sensor precipitation estimates at fine scales, J. Hydrometeorol., 8(1), 38–55, 2007. </reference>
		<reference numeration="4" content_type="text"> Kummerow, C., Hong, Y., Olson, W. S., Yang, S., Adler, R. F., Mccollum, J., Ferraro, R., Petty, G., and Wilheit, T. T.: The evolution of the Goddard Profiling Algorithm (GPROF) for rainfall estimation from passive microwave sensors, J. Appl. Meteorol., 40, 1801–1820, 2001. </reference>
		<reference numeration="5" content_type="text"> Lionello, P., Malanotte-Rizzoli, P., Boscolo, R., et al. : The Mediterranean Climate: An overview of the main characteristics and issues, Mediterranean Climate Variability, Elsevier B. V., 1–26, 2006a. </reference>
		<reference numeration="6" content_type="text"> Lionello, P., Bhend, J., Buzzi, A., et al. : Cyclones in the Mediterranean region: climatology and effects on the environment, Mediterranean Climate Variability, Elsevier B. V., 325–372, 2006b. </reference>
		<reference numeration="7" content_type="text"> Trigo, R. M., Xoplaki, E., Zorita, E., et al.: Relationship between variability in the Mediterranean region and mid-latitude variability, Mediterranean Climate Variability, Elsevier B. V., 179–226, 2006. </reference>
		<reference numeration="8" content_type="text"> Trigo, I. F.: Climatology and interannual variability of storm-tracks in the Euro-Atlantic sector: a comparison between ERA-40 and NCEP/NCAR reanalysis, Clim. Dynam., 26, 127–143, 2006. </reference>
		<reference numeration="9" content_type="text"> Xoplaki, E., Gonzalez-Rouco, J. F., Luterbacher, J., and Wanner, H.: Wet season Mediterranean precipitation variability: influence of large-scale dynamics and trends, Clim. Dynam., 23, 63–78, 2004. </reference>
		<reference numeration="10" content_type="text"> Yang, S. and Smith, E. A.: Convective – stratiform precipitation variability at seasonal scale from eight years of TRMM observations: Implications for multiple modes of diurnal variability, J. Climate, 21, 4087–4114, 2008. </reference>
	</references>
</article>

