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Finding an effective method to upscale or downscale hydrological processes is the central concern in hydrological research. The aim of this paper is to investigate a powerful, regulated relationship between runoff and catchment area, and establish the runoff scale transfer model for Gongga Mountain in China. We chose a series of catchments 5 in which the contributing areas ranged from 0.41 km 2 to 80.5 km 2 to monitor the hymeasure. One common similarity measure is spatial proximity, based ondoi:10.5194/hessd-7-2157-2010 fatcat:ysy64s5oorhmlkpjbnlltgw6ie