Technical Papers
Jan 11, 2012

Using Hydrologic Simulation to Explore the Impacts of Climate Change on Runoff in the Huaihe River Basin of China

Publication: Journal of Hydrologic Engineering
Volume 18, Issue 11

Abstract

Climate change has become an environmental issue of utmost importance, and one that will challenge existing water resource management practices in many ways. The Huaihe River, one of China’s major rivers, is frequently subject to flooding and drought and, for the purposes of assessing the implications of climate change on water resources in the Huaihe River Basin, the variable infiltration capacity (VIC) model with a resolution of 0.5°×0.5° was calibrated using data from 11 well-gauged subbasins. The model parameters from the well-gauged stations were then transferred to poorly gauged areas according to similarities in, for example, climate conditions and soil texture. The calibrated VIC model was subsequently used to study the potential impacts of three climate change scenarios on basin runoff, taking projected runoff for 1961–1990 as the baseline. In general, the results showed that although the annual runoff will likely increase across the basin under the different scenarios, regional flooding and regional shortage in water resources will be exacerbated under the impacts of global warming.

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Acknowledgments

This study has been financially supported by the National Basic Research Program of China (grant 2010CB951103), the International Science & Technology Cooperation Program of China (grant 2010DFA24330), and the ACCC project funded by DFID, SDC, and DECC. Thanks also to the anonymous reviewers and editors.

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Information & Authors

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Published In

Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 18Issue 11November 2013
Pages: 1393 - 1399

History

Received: May 23, 2011
Accepted: Jan 9, 2012
Published online: Jan 11, 2012
Discussion open until: Jun 11, 2012
Published in print: Nov 1, 2013

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Authors

Affiliations

J. Y. Zhang
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China.
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China (corresponding author). E-mail: [email protected]
T. C. Pagano
Commonwealth Scientific and Industrial Research Organization, Land and Water, Melbourne, Victoria, Australia.
J. L. Jin
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China.
C. S. Liu
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China.
R. M. He
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China.
Y. L. Liu
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, Jiangsu Province, China; and Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, Jiangsu Province, China.

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