<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Oikonomou, C.</style></author><author><style face="normal" font="default" size="100%">H. A. Flocas</style></author><author><style face="normal" font="default" size="100%">M. Hatzaki</style></author><author><style face="normal" font="default" size="100%">Nisantzi, A.</style></author><author><style face="normal" font="default" size="100%">Asimakopoulos, D.N.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Relationship of extreme dry spells in Eastern Mediterranean with large-scale circulation</style></title><secondary-title><style face="normal" font="default" size="100%">Theoretical and Applied Climatology</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Atlantic Ocean</style></keyword><keyword><style  face="normal" font="default" size="100%">Atlantic Ocean (North)</style></keyword><keyword><style  face="normal" font="default" size="100%">atmospheric circulation</style></keyword><keyword><style  face="normal" font="default" size="100%">canonical analysis</style></keyword><keyword><style  face="normal" font="default" size="100%">dry season</style></keyword><keyword><style  face="normal" font="default" size="100%">Europe</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean Region</style></keyword><keyword><style  face="normal" font="default" size="100%">summer</style></keyword><keyword><style  face="normal" font="default" size="100%">Synoptic meteorology</style></keyword><keyword><style  face="normal" font="default" size="100%">teleconnection</style></keyword><keyword><style  face="normal" font="default" size="100%">winter</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.scopus.com/inward/record.url?eid=2-s2.0-77049111799&amp;partnerID=40&amp;md5=17676bdcfd1efa1bc4422e41341c5036</style></url></web-urls></urls><number><style face="normal" font="default" size="100%">1</style></number><volume><style face="normal" font="default" size="100%">100</style></volume><pages><style face="normal" font="default" size="100%">137-151</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The relationship of prolonged dry spells in Eastern Mediterranean with large-scale surface and upper circulation is investigated on seasonal basis with the aid of the Singular-Value Decomposition Analysis (SVDA) for the period 1958-2000. The study was based on daily precipitation data of 56 stations, evenly distributed over Eastern Mediterranean region. Extreme dry spells are defined using the CDD index (maximum number of consecutive dry days). It was found that teleconnection patterns centered over Northern Atlantic and northern Europe seem to affect the duration of the longest dry spells over the Eastern Mediterranean, while surface synoptic scale systems in Northern Africa play a substantial role. The SVDA results compare well with the corresponding results of Canonical Correlation Analysis (CCA), mainly for the surface circulation during winter and summer. © Springer-Verlag 2009.</style></abstract><notes><style face="normal" font="default" size="100%">cited By (since 1996)5</style></notes></record></records></xml>