text: The higher-resolution HadGEM3 simulations project consistent increases in temperature-related 
  extremes, with larger changes at 2°C compared to 1.5°C and local changes being larger than the 
  global annual mean. There is a higher degree of spatial variation in our projections compared 
  with CMIP5-based studies. 
  
  In the model projections examined here, changes relating to the water cycle are complex, both 
  in their geographical pattern and in the variation between different models. The length of ﬂooding 
  events generally increases across world in all models, but maximum rainfall can either increase or 
  decrease depending on locations. Global patterns of increase and decrease show some consistency 
  between the different GWLs, but also some local differences. Worldwide, most impacts broadly 
  tend to increase with global warming in most areas. For global mean changes, even when the sign 
  of change is uncertain, individual realizations generally show reduced impact at 1.5°C compared 
  with 2°C. However, this does not always hold even at the scale of major global river basins. 
  
  Vulnerability to food insecurity increases more at 2°C global warming than 1.5°C in 
  approximately three-quarters of countries assessed. The vulnerability increase can arise from 
  increases in either ﬂooding or drought. Reduced drought leads to decreased vulnerability in a 
  limited number of cases. 