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G. T. Aronica and B. Bonaccorso

cover a reasonable number of GCM grid cells ( Arora and Boer 2001 ; Mirza 2002 ; Hamlet and Lettenmaier 2007 ; Gain et al. 2011 ). On the other hand, GCMs are inadequate to simulate regional and local climate change when dealing with spatial scale of ~1000 km 2 or finer, as in most common hydrological applications. Therefore, downscaling or disaggregating techniques (both statistical methods and nested RCMs) are generally used to transfer climate data from GCM scales to the river basin scale

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