<?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%">Calafat, F.M., Francisco.calafat@noc.ac.uk</style></author><author><style face="normal" font="default" size="100%">E. Avgoustoglou</style></author><author><style face="normal" font="default" size="100%">Jordà, G.</style></author><author><style face="normal" font="default" size="100%">Flocas, H.</style></author><author><style face="normal" font="default" size="100%">Zodiatis, G.</style></author><author><style face="normal" font="default" size="100%">Tsimplis, M.N.</style></author><author><style face="normal" font="default" size="100%">J. Kouroutzoglou</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The ability of a barotropic model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Geophysical Research: Oceans</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.scopus.com/inward/record.uri?eid=2-s2.0-84915748625&amp;doi=10.1002%2f2014JC010360&amp;partnerID=40&amp;md5=7fc901255122aad0ab735951901075e9</style></url></web-urls></urls><number><style face="normal" font="default" size="100%">11</style></number><volume><style face="normal" font="default" size="100%">119</style></volume><pages><style face="normal" font="default" size="100%">7840-7853</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record></records></xml>