<?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%">Flocas, H.A.a</style></author><author><style face="normal" font="default" size="100%">Hatzaki, M.a c</style></author><author><style face="normal" font="default" size="100%">Tolika, K.b</style></author><author><style face="normal" font="default" size="100%">Anagnostopoulou, C.b</style></author><author><style face="normal" font="default" size="100%">Kostopoulou, E.c</style></author><author><style face="normal" font="default" size="100%">Giannakopoulos, C.c</style></author><author><style face="normal" font="default" size="100%">Kolokytha, E.a</style></author><author><style face="normal" font="default" size="100%">Tegoulias, I.b</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Ability of RCM/GCM couples to represent the relationship of large scale circulation to climate extremes over the Mediterranean region</style></title><secondary-title><style face="normal" font="default" size="100%">Climate Research</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">atmospheric circulation</style></keyword><keyword><style  face="normal" font="default" size="100%">atmospheric general circulation model</style></keyword><keyword><style  face="normal" font="default" size="100%">Atmospheric movements</style></keyword><keyword><style  face="normal" font="default" size="100%">canonical analysis</style></keyword><keyword><style  face="normal" font="default" size="100%">Circulation patterns</style></keyword><keyword><style  face="normal" font="default" size="100%">climate modeling</style></keyword><keyword><style  face="normal" font="default" size="100%">Climate models</style></keyword><keyword><style  face="normal" font="default" size="100%">Climatology</style></keyword><keyword><style  face="normal" font="default" size="100%">correspondence analysis</style></keyword><keyword><style  face="normal" font="default" size="100%">data set</style></keyword><keyword><style  face="normal" font="default" size="100%">Ensembles</style></keyword><keyword><style  face="normal" font="default" size="100%">Extreme climate indices</style></keyword><keyword><style  face="normal" font="default" size="100%">global climate</style></keyword><keyword><style  face="normal" font="default" size="100%">Global climate models</style></keyword><keyword><style  face="normal" font="default" size="100%">Large scale circulation</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean environment</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean Region</style></keyword><keyword><style  face="normal" font="default" size="100%">precipitation (climatology)</style></keyword><keyword><style  face="normal" font="default" size="100%">RCCA</style></keyword><keyword><style  face="normal" font="default" size="100%">regional climate</style></keyword><keyword><style  face="normal" font="default" size="100%">Regional climate models</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.scopus.com/inward/record.url?eid=2-s2.0-79957647413&amp;partnerID=40&amp;md5=e438d55e8eb41e95d3ebf5ef481a9ee6</style></url></web-urls></urls><number><style face="normal" font="default" size="100%">3</style></number><volume><style face="normal" font="default" size="100%">46</style></volume><pages><style face="normal" font="default" size="100%">197-209</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The objective of this study was to explore the ability of 3 regional climate models (RCMs), CNRM-Aladin, C4I-RCA3 and KNMI-RACMO along with their parental global climate models (GCMs), ARPEGE and ECHAM5, to represent the relationship between large-scale atmospheric circulation and climate extremes in the Mediterranean region. Subsequently, an evaluation and inter-comparison of these 3 RCM/GCM couples for the present climate was performed. For this purpose, the Regularised Canonical Correlation Analysis (RCCA) was employed and 4 extreme climate indices of temperature and precipitation were used to define extreme events over the study region. The evaluation of these relationships was carried out against gridded observational and reanalysis datasets. It was found that the observed upper air large scale patterns related to climate extremes in the Mediterranean are not very well reproduced by the RCM/GCM couples in all seasons. In addition, in many cases, the coupled models display patterns of extreme climate indices which are not consistent with the accompanied upper level circulation. Furthermore, all coupled models display substantial deficiencies in simulating precipitation extremes. In the case of summer data, the ability of all 3 models is limited, possibly because the strength of the large-scale atmospheric flow decreases, the control exerted by the lateral boundary conditions is weaker, and the nested models are mainly governed by local processes. © Inter-Research 2011.</style></abstract><notes><style face="normal" font="default" size="100%">cited By (since 1996)1</style></notes></record></records></xml>