## Abstract Afforestation has been suggested as a means of improving soil and water conservation in northβwestern China, especially on the Loess Plateau. Understanding of the hydrological responses to afforestation will help us develop sustainable watershed management strategies. A study was conduc
Modelling the impact of afforestation on average annual streamflow in the Loess Plateau, China
β Scribed by Xiao Ping Zhang; Lu Zhang; Tim R. McVicar; Tom G. Van Niel; Ling Tao Li; Rui Li; QinKe Yang; Liang Wei
- Publisher
- John Wiley and Sons
- Year
- 2008
- Tongue
- English
- Weight
- 431 KB
- Volume
- 22
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.6784
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
To prevent severe soil erosion and to ensure sustainable development, the Chinese Central Government mandated in 1999 that forest cover would be significantly increased in the Loess Plateau, China. It is important to assess the subsequent impact on streamflow and its spatial distribution in the region. The water balance model of et al. (2001)Zhang et al. (2001) was used in this study, and the results showed that the model was able to accurately simulate average annual evapotranspiration (ET), but not average annual streamflow when compared with streamflow measurements from 38 hydrologic stations in the coarse sandy hilly catchments (CSHC) in the Loess Plateau. The model was then calibrated using the measured streamflow, and the index of agreement increased from 0Β·21 to 0Β·63, the relative error and root mean square error decreased from 42Β·7 and 17Β·2 to 18Β·0% and 7Β·9 mm, respectively. Hierarchical cluster analysis and stepwise regression were employed to regionalize the optimized model parameter and relate it to the dryness index and forest cover. Once calibrated, the water balance model was used to assess the impacts of two plantation scenarios on streamflow. The two plantation scenarios assume nearly 5Β·8 and 10Β·1% of the study area can be planted with trees. It was predicted that streamflow from the region will decrease by 5Β·5 and 9Β·2% under the two plantation scenarios. The rate of streamflow reduction decreased from southeast to northwest mainly due to decreasing precipitation. Copyright Β© 2007 John Wiley & Sons, Ltd.
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