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The Corinthian Gulf is a narrow sea-level passage surrounded by a steepcomplex topography that consists of high mountains as well as elevated and sea-levelgaps and straits. The complex terrain is expected to affect the wind flow in thearea that often experiences high winds, with important consequences on thecommercial and recreational activities over the gulf's maritime area. For thatreason, a model-based study of the wind regime over the Corinthian Gulf hasbeen created, as observational data over the area are recent and spatiallysparse. Analysis of 5 yr of data from the fifth-generation Penn State/NCAR mesoscale model (MM5) model reveals that the wind regime of the gulf is greatly influenced by the topography. Easterly windsoccur more frequently and are stronger in the maritime area in the westernedge of the gulf, with a frequency of occurrence on the order of 70%.Moreover, the most intense wind events at this area occur during the winterseason (December, January, and February). Finally the paper also provides adiscussion on the synoptic patterns, which lead to the strongest wind eventsin the studied area

A model-based study of the wind regime over the Corinthian Gulf