“…It is common to adopt the outputs of general circulation models (GCMs) with predefined scenarios to forecast future weather conditions and to assess their impacts on regional water resources (Arora, ; Timbal et al, ; Alkuwari et al, ; Beecham et al, ; Mahmood and Babel, ; Rashid et al, ; Tofiq and Guven, ). However, GCM outputs are represented in a grid ranging from 150–300 km in size, which is too spatially coarse for regional weather and water resource conditions, and further limits their direct regional application (Arora, ; Timbal et al, ; Beecham et al, ; Manor and Berkovic, ; Su et al, ).…”