The exact determination of the
climate evolution is of most importance as well for theoretical purposes as for practical
applications. Moreover, if the change-point way of evolution of the climate has already
been evidenced in the nineteen-fifties (Sneyers 1997), Monte-Carlo experiments have shown
the limits of change-point detection (Easterling and Peterson
1995).
The purpose of this paper is to
summarise the principles of change-point detection for their complete determination and
their exact significance as alternative assumption to randomness.
The analysis of the Casablanca
temperature series is given for illustrating the method.