Relative anomalies were used. The ratio was calculated as follows: r ¼ hxifuture=hxipresent , where x is the variable of interest. Afterwards the ratio was applied to the SAFRAN series of present climate.
Relative anomalies were used. The ratio was calculated as follows:r ¼ hxifuture=hxipresent , where x is the variable of interest.Afterwards the ratio was applied to the SAFRAN series of presentclimate.