Technical Papers
Aug 5, 2011

Impacts of Land-Use and Climate Changes on Hydrologic Processes in the Qingyi River Watershed, China

Publication: Journal of Hydrologic Engineering
Volume 18, Issue 11

Abstract

The impacts of human-induced land-use and climate changes on hydrologic processes have become a great challenge and attracted widespread attention of many researchers. Dramatic changes in land use and climate have occurred in the mountainous Qingyi River watershed in southwest China in the last three decades. Variable infiltration capacity (VIC), a large-scale hydrologic model, was used in this study to assess the impacts of land-use and climate changes on surface runoff, base flow, streamflow, and evapotranspiration (ET) of this watershed. The analysis for this study includes (1) investigation of change in historical land-use patterns, (2) detection of climate change (precipitation and mean temperature), and (3) simulation and assessment of hydrologic responses to these changes. The Mann-Kendall test was used to identify the long-term monotonic trends in precipitation and temperature for the period of 1980–2005. The results suggest no significant change in annual precipitation and a significant increase in annual temperature, particularly in February, April, July, and September. The analysis of three land-use maps reveals that the conversions between forest and shrubland/grassland were the predominant land-use change over the past three decades. Hydrologic simulations show that the influence of climate change on hydrologic processes was stronger than those of land-use change. Monthly variation of the river flow was mainly attributed to seasonal variation in precipitation. However, ET responded significantly to the land-use change in several subwatersheds where single land cover conversion occurred dominantly. The decrease in surface runoff and base flow caused by climate change was enhanced by changes in land use, whereas the reduction in ET was offset by reforestation over the study period. Furthermore, the impact of deforestation or reforestation on hydrologic processes was more significant in the dry season than other seasons. The results from this study can be a useful reference for decision making in land-use planning and water resource managements in this region.

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Acknowledgments

This study has been supported by the National Natural Science Foundation (41030636, 50879017) and the National Science and Technology Support Programme (2008BAB29B08-02). The authors also would like to give special thanks to Professor Zhongbo Yu for his help with the comments and English writing.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 18Issue 11November 2013
Pages: 1495 - 1512

History

Received: Aug 28, 2010
Accepted: Aug 3, 2011
Published online: Aug 5, 2011
Discussion open until: Jan 5, 2012
Published in print: Nov 1, 2013

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Yangyang Liu [email protected]
Ph.D. Candidate, College of Hydrology and Water Resources, Hohai Univ., No. 1, Xikang Rd., Nanjing 210098, China (corresponding author). E-mail: [email protected]
Xingnan Zhang [email protected]
Deputy Director, National Engineering Research Center of Water Resources Efficient Utilization and Engineering Safety, Hohai Univ., No. 1, Xikang Rd., Nanjing 210098, China. E-mail: [email protected]
Dazhong Xia [email protected]
Lecturer, College of Hydrology and Water Resources, Hohai Univ., No. 1, Xikang Rd., Nanjing 210098, China. E-mail: [email protected]
Jinsheng You [email protected]
School of Natural Resources, Univ. of Nebraska, Lincoln, NE 68583. E-mail: [email protected]
Yanshu Rong [email protected]
College of Hydrology and Water Resources, Hohai Univ., No. 1, Xikang Rd., Nanjing 210098, China. E-mail: [email protected]
Mohamad Bakir [email protected]
College of Hydrology and Water Resources, Hohai Univ., No. 1, Xikang Rd., Nanjing 210098, China. E-mail: [email protected]

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