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A simple transfer function method is used to spatially downscale extreme precipitation and temperature indices of six GCMs (CNRM-CM3, GFDL-CM2.1, INM-CM3.0, IPSL-CM4, MIROC3.2_M and NCAR-PCM) under three emission scenarios (A1B, A2, B1) from grid outputs to target station to project their potential spatiotemporal changes on the Loess Plateau of China during the 21st century. GCMs project that extreme...
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