text: (a) Climate-change impacts at 2°C global warming 
  
  For 2°C global warming, the ensemble-mean increase in annual daily maximum temperature was 
  above 2°C for most of the land surface, with the exception of the Indian subcontinent, most of 
  Australia and Antarctica (ﬁgure 2). The increase was higher still in many regions; most of North 
  America, much of China and north Asia, northwestern South America and all of Europe. In the 
  northern and eastern USA and much of northern and western Europe, the annual daily maximum 
  temperature increased by over 4°C for 2°C global warming. The global mean TXx increased by 
  more than 2°C in all ensemble members (table 5), so the maximum temperature warming more 
  than the global annual mean is a consistent result across all projections here, as found in previous 
  studies with other models [9] (table 5). 
  
  The different ensemble members give somewhat different results at regional scales, although 
  there is a strong consensus on the temperature extremes examined here becoming warmer. In 
  the simulations driven by SSTs and SICs from the two IPSL CMIP5 models, most of the global 