2010Unpublished venueRequires access

Runoff Simulation and Analysis in Upstream Dagu River Watershed Using a Distributed Hydrological Model

Xiang Pu, Zhe Liu, Huiwang Gao, Yunjun Yu

Open publisher page 1 citations

Abstract

The distributed hydrological model, SWAT, was used to study the seasonal and interannual variation of the runoff in upstream Dagu River watershed and the governing processes as well. The model output is sensitive to five parameters (e.g., Cn2, Esco, and Sol_Awc). The modeled result shows maximum monthly runoff occurring in August and minimum in February, consistent with the observation. The average annual runoff depth is about 83 mm, with strong interannual variability. The runoff depth was deep in the eastern and western areas, while it is relatively shallow in the southern and northern area. Furthermore, the impact of land use/ land cover change on runoff yield was also discussed.

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What this paper is about

The distributed hydrological model, SWAT, was used to study the seasonal and interannual variation of the runoff in upstream Dagu River watershed and the governing processes as well. The model output is sensitive to five parameters (e.g., Cn2, Esco, and Sol_Awc). The modeled result shows maximum monthly runoff occurring in August and minimum in February, consistent with the observation. The average annual runoff depth is about 83 mm, with strong interannual variability. The runoff depth was deep in the eastern and western areas, while it is relatively shallow in the southern and northern area. Furthermore, the impact of land use/ land cover change on runoff yield was also discussed.

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Available abstract

The distributed hydrological model, SWAT, was used to study the seasonal and interannual variation of the runoff in upstream Dagu River watershed and the governing processes as well. The model output is sensitive to five parameters (e.g., Cn2, Esco, and Sol_Awc). The modeled result shows maximum monthly runoff occurring in August and minimum in February, consistent with the observation. The average annual runoff depth is about 83 mm, with strong interannual variability. The runoff depth was deep in the eastern and western areas, while it is relatively shallow in the southern and northern area. Furthermore, the impact of land use/ land cover change on runoff yield was also discussed.

Key concepts: Surface runoff, Watershed, Hydrology (agriculture), Environmental science, Vflo, Runoff curve number, Land cover, SWAT model

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