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6437842 
Journal Article 
The regional variation in climate elasticity and climate contribution to runoff across China 
Yang, H; Qi, Jia; Xu, X; Yang, D; Lv, H 
2014 
Yes 
Journal of Hydrology
ISSN: 0022-1694 
Elsevier 
517 
Elsevier 
607-616 
WOS:000340977000052 
The climate elasticity of runoff is an important indicator that is used to quantify the relationship between changes in runoff and changes in climate variables. It is a function of both climate and catchment characteristics. Recently, Yang and Yang (2011) proposed an analytical derivation of climate elasticity (YY2011), in which a parameter n was used to represent the impact of the catchment characteristics. In China, both climate and catchment characteristics have large spatial variations. To understand the spatial variation of hydrologic response to climate change, this paper divided China into 210 catchments, further calculated the parameter n, and then estimated the climate elasticity and evaluated the contribution of climate change to runoff for each catchment. The results show that n ranges from 0.4 to 3.8 (with a mean of 1.3 and a standard deviation of 0.6), which has a logarithmic relationship with catchment slope; the precipitation elasticity ranges from 1.1 to 4.8 (with a mean of 1.9 and a standard deviation of 0.6), which shows a large regional variation, smaller values (1.1-2.0) mainly appearing in Southern China, the Songhua River basin and the Northwest, and larger values (2.1-4.8) mainly appearing in the Hai River basin, the Liao River basin and the Yellow River basin. In addition, climate contribution to runoff exhibits a large regional variation, the largest positive values (1.1-3.1%/a) occurring in the Northwest, the largest negative values (-1.0 to -0.5%/a) occurring in the Hai River basin and the middle reach of the Yellow River basin. In theory, the YY2011 method is a first-order approximation. The approximation underestimates the precipitation (P) contribution to runoff when P increases and overestimates that when P decreases, and the relative error has a median of 3% and a maximum of 20% when 10% precipitations change in those catchments of China. 
Climate elasticity; Runoff; Budyko hypothesis; Precipitation; Potential evaporation; Error analysis