## Abstract The hydrological response to climate change in the Tarim River Basin was investigated by analysing the hydrological, temperature and precipitation data of the past 50 years. The long‐term trend of the hydrological time‐series, including air temperature, precipitation, and streamflow, wa
Impacts of climate change and human activities on surface runoff in the Dongjiang River basin of China
✍ Scribed by Dedi Liu; Xiaohong Chen; Yanqing Lian; Zhanghua Lou
- Publisher
- John Wiley and Sons
- Year
- 2010
- Tongue
- English
- Weight
- 192 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.7609
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
Observed rainfall and flow data from the Dongjiang River basin in humid southern China were used to investigate runoff changes during low‐flow and flooding periods and in annual flows over the past 45 years. We first applied the non‐parametric Mann–Kendall rank statistic method to analyze the change trend in precipitation, surface runoff and pan evaporation in those three periods. Findings showed that only the surface runoff in the low‐flow period increased significantly, which was due to a combination of increased precipitation and decreased pan evaporation. The Pettitt–Mann–Whitney statistical test results showed that 1973 and 1978 were the change points for the low‐flow period runoff in the Boluo sub‐catchment and in the Qilinzui sub‐catchment, respectively. Most importantly, we have developed a framework to separate the effects of climate change and human activities on the changes in surface runoff based on the back‐propagation artificial neural network (BP‐ANN) method from this research. Analyses from this study indicated that climate variabilities such as changes in precipitation and evaporation, and human activities such as reservoir operations, each accounted for about 50% of the runoff change in the low‐flow period in the study basin. Copyright © 2010 John Wiley & Sons, Ltd.
📜 SIMILAR VOLUMES
## Abstract Located in the Loess Plateau of China, the Wuding River basin (30 261 km^2^) contributes significantly to the total sediment yield in the Yellow River. To reduce sediment yield from the catchment, large‐scale soil conservation measures have been implemented in the last four decades. The
## Abstract Potential climate change is expected to produce substantial effects on the hydrological cycle. In a companion paper (Burlando P, Rosso R. __Hydrological Processes__ this issue) the effects on precipitation have been discussed, with particular attention being given to significant changes
## Abstract The Yiluo River is the largest tributary for the middle and lower reaches of the Yellow River below Sanmenxia Dam. Changes of the hydrological processes in the Yiluo River basin, influenced by the climatic variability and human activities, can directly affect ecological integrity in the
## Abstract In this study we developed an impact factor formula (IFF) to quantitatively attribute separately the impacts of climate change and local human activities on hydrological response (i.e. run‐off) in a sub‐basin of Yellow River for the period 1950–2000. Using the daily climatic data, we fi