Fig. 5.

Scaling of R95p rainfall intensity for the Indian region. Panels (a) and (b) depict the scaling for mid-century and end-century scenarios, respectively. Panels (c) and (d) illustrate the variation in rainfall intensities with surface air temperature for mid-century and end-century periods, respectively. Different coloured lines represent the non-parametric fitting using LOWESS smoothing for various climate change scenarios. In (a) and (b), three reference lines indicate typical CC scaling (dots), 1.5 times CC scaling (dash) and 2 times CC scaling (dot-dash). The peak-point temperature for each scenario is highlighted in (c) and (d).