Runoff is one of the key driving forces of watershed hydrological cycle processes. Quantifying the relative impacts of climate change and human activities on runoff change is critical to clarifying the mechanisms of watershed hydrological responses. This study analyses the characteristics of hydrological changes in the Jialing River Basin based on datasets from 1957 to 2017. The degree of runoff change was then quantified with the aid of the IHA-RVA method. By establishing the Budyko model and comparing the Slope change ratio of the accumulative quantity, the contribution rate of climate change and human activities to runoff change was quantified. The result: (1) except for Qujiang River Basin, the average annual runoff of other basins showed a significant downward trend. 1985 was chosen as the abrupt change year. (2) The overall flow alteration in the basin is 50.87%, which is close to the height change. (3) The impacts of climate change and human activities on runoff before and after the abrupt change have certain spatial differences. Human activities are the main influence factors, of which the contribution rates to the Fu River Basin, the mainstream of Jialing River, Bailong River Basin, and Qu River Basin are 64.57, 66.31, and 74.17% respectively.

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