text: members at any given date. Since speciﬁc levels of global warming such as 1.5°C or 2°C were 
  reached at different times in the different ensemble members, according to the SST forcings used, 
  any given level of global warming could be associated with different radiative forcings in different 
  ensemble members. In any given ensemble member at any speciﬁc level of global warming, the 
  CO2 concentration and SSTs were the same as in the driving CMIP5 model at that GWL. Land 
  cover was ﬁxed in this simulation—there was no dynamic vegetation nor any time-dependent 
  anthropogenic land use change. 
  Some comparison of the higher-resolution atmospheric simulations with the original CMIP5 
  simulations, is provided by Wyser*et al.*[20]. 
  
  (b) Temperature and precipitation extremes: the ClimPACT indices 
  
  To quantify changes in weather extremes projected in our climate simulations, we calculated 
  a number of indices designed to be relevant to sector-speciﬁc impacts using an established 
  methodology, ClimPACT [21] (table 1) 
  
  (c) Food security: the Hunger and Climate Vulnerability Index 