This paper aims at comparing the evolution from 1950 to 2010 of the average annual minimum temperatures of 34 stations in the French Mediterranean region with the mean global average temperatures with a significant rise in temperatures between 1950 and 2012 divided into two periods, first a slowly descending one till the 70’s followed by a second ascending up quickly till the end of the century (Stork et al., 2013). The environment of the French stations has been determined from georeferenced documents of different dates. Their linear evolution has been studied from a dual linear regression starting one at the beginning of the period, the other at the end with the aim of determining if it presented a succession of two periods with different evolution separated by a rupture.