The Mediterranean is a miniature ocean where most of the processes documented in the global ocean are encountered (Lejeusne et al., 2010). Indeed, important global features are present in it, but on smaller spatial and temporal scales (Bethoux et al., 1999) such as the thermohaline circulation forced by dense water formation in winter. In addition, several features of the Mediterranean make it a hotspot of marine biodiversity (Coll et al., 2010) and potentially vulnerable to climate change.At regional scale, the Mediterranean Sea plays a role of sentinel with regard to global warming since it is very sensitive to climate change (Giorgi, 2006). Indeed, the Mediterranean Sea was one of the first ocean places where a warming trend was observed in the deep-water temperatures in the western basin and attributed to global warming (Bethoux et al., 1990). The Mediterranean Sea Surface Temperature (SST) has experienced an intensive and continuous warming since the mid-1980s, which is expected to increase throughout the 21st century under present climate scenarios (Somot et al., 2008). Several studies have shown an increase of the mean Mediterranean SST in the last three decades. Based on the 4 km Advanced Very High Resolution Radiometer (AVHRR) Pathfinder SST data set, Nykjaer ( 2009) estimated a mean warming trend of 0.03 ± 0.008°C/year in the western Mediterranean Sea and 0.05 ± 0.009°C/year in the eastern basin from 1985 to 2006. Similar results were found by (López García & Camarasa, 2011) from 1985. Based on Reynolds' SST reanalysis (Reynolds et al., 2007, Shaltout and Omstedt (2014) found a mean warming trend of 0.035 ± 0.007°C/year during a 31-year period (1982-2012) over the Mediterranean Sea. And recently,