text: all members (ﬁgure 12). This is not the case for the precipitation and run-off results; for those 
  quantities, there is substantial overlap in the ranges of changes at 2°C and 1.5°C, so there is not a 
  consistent picture of how much wetter or drier the world is projected to be in this ensemble, even 
  though it involves a single atmosphere model. 
  
  For TXx, the difference between 2°C and 1.5°C global warming is larger than the 0.5°C 
  difference in global mean temperature across most of the land surface in all ensemble members 
  (ﬁgure 14). Although some ensemble members simulate local temperatures to be higher at 1.5°C 
  global warming than 2°C in some small regions, these are relatively localized and most regions 
  are cooler at 1.5°C global warming than 2°C. In many regions, the difference is between 0.5°C and 
  1.0°C, but many other regions see larger differences. In several ensemble members, the difference 
  is 1.5°C, 2°C or larger in large parts of North America, South America, Europe and China. 
  For example, over parts of Europe, where annual maximum daily temperature was projected 
  to increase by over 5°C for a 2°C global warming, the local increase is limited to 3–4°C for 
  1.5°C global warming. Limiting global warming by half a degree Celsius would, therefore, limit 
  maximum temperatures by three or four times as much in those areas (ﬁgure 14). 