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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 11
Hydrol. Earth Syst. Sci., 17, 4471–4480, 2013
https://doi.org/10.5194/hess-17-4471-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 17, 4471–4480, 2013
https://doi.org/10.5194/hess-17-4471-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 12 Nov 2013

Research article | 12 Nov 2013

Responses of natural runoff to recent climatic variations in the Yellow River basin, China

Y. Tang1, Q. Tang1, F. Tian2, Z. Zhang3, and G. Liu1,4 Y. Tang et al.
  • 1Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
  • 2State Key Laboratory of Hydroscience and Engineering & Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China
  • 3College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
  • 4University of Chinese Academy of Sciences, Beijing 100049, China

Abstract. The zero-flow phenomenon appeared frequently in the lower reaches of the Yellow River in China in the 1990s, whereas it has almost disappeared in recent years. The disappearance of the zero-flow phenomenon should be mainly attributed to the recent water management practices. However, little is known about the effects of recent climatic variations on natural runoff. In this study, we investigated the impacts of climatic variations on natural runoff above the Huayuankou station. The results indicate that there was little increase in precipitation, but substantial recovery of natural runoff in the recent period (2003–2011) compared with the low-flow period (1991–2002). The recent precipitation was slightly greater (∼2% of the baseline precipitation in 1960–1990) than precipitation in the low-flow period. However, the recent natural runoff was much larger (∼14% baseline runoff) than runoff in the low-flow period. The runoff reduction in the low-flow period was mainly caused by precipitation decrease. In the recent period, precipitation accounted for a runoff reduction (∼21% baseline runoff), whereas net radiation, wind speed, air temperature, and relative humidity accounted for a runoff increase (∼7.5% baseline runoff). The spatial pattern of the climatic variation is a factor influencing the response of runoff to climatic variations. The reduction in runoff induced by precipitation change was offset up to half by the impacts of changes in net radiation and wind speed at most sub-basins in the recent period.

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