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Zhao Yang, Francina Dominguez, Hoshin Gupta, Xubin Zeng, and Laura Norman

a high-resolution simulation that does not require a convective parameterization and so is able to more accurately represent convective events during the monsoon season; that is, our simulations are at a 2-km resolution, while Georgescu et al. (2012 , 2013) use 20-km resolution. In the next section, we introduce the numerical model and experimental design. Section 3 presents and discusses results from two land-use scenarios and reports additional analysis regarding the potential impacts of

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G. Strandberg and E. Kjellström

. 2016 ) is used to perform the climate simulations. RCA4 and its predecessors, RCA, RCA2, and RCA3, have been extensively used and evaluated in studies of present and future climate (e.g., Rummukainen et al. 2001 ; Räisänen et al. 2004 ; Kjellström et al. 2011 ; Nikulin et al. 2011 ). Also, RCA3 has been used in palaeoclimatological applications for downscaling global model results for the last millennium ( Graham et al. 2009 ; Schimanke et al. 2012 ), for parts of the Marine Isotope Stage 3

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