polar

, and

DOI: 10.3369/tethys.2011.8.04

pp.: 31 - 42

Abstract

This work analyzes the energy teleconnections observed between Sea Surface Temperature anomalies in the North Atlantic and the cyclogenesis of the western Mediterranean basin. The basin has a high edge and in its central part there is a warm and evaporating sea that is crucial for energy exchanges that are key for its autarkic climatology. This could be the reason for not having observed any signification in the teleconnections between Mediterranean rainfalls and the North Atlantic Oscillation index.

References



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Partially funded through grants CGL2007-29820-E/CLI, CGL2008-02804-E/, CGL2009-07417-E and CGL2011-14046-E of the Spanish Ministry of Science and Innovation



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