Yu Haichao, Zhang Yang, Ma Jinzhu, et al. Variation of Observed and Natural Runoff of Yellow River from 1969 to 2018[J]. Bulletin of Soiland Water Conservation, 2020, 40(5): 1-7.
DOI:
Yu Haichao, Zhang Yang, Ma Jinzhu, et al. Variation of Observed and Natural Runoff of Yellow River from 1969 to 2018[J]. Bulletin of Soiland Water Conservation, 2020, 40(5): 1-7. DOI: 10.13961/j.cnki.stbctb.2020.05.001.
Variation of Observed and Natural Runoff of Yellow River from 1969 to 2018
[Objective] The variation of the observed runoff and natural runoff of the Yellow River was analyzed to explore the impact of human activities on runoff in the study area.[Methods] Based on the natural runoff and observed runoff of eight hydrological stations in the main stream of the Yellow River from 1969 to 2018
the variation of the observed natural runoff in the last 50 years was analyzed using a Mann-Kendall trend test and mutant test. In addition
the impact of human activities on runoff was considered based on the water consumption data of each region in the last 15 years.[Results] ① The observed runoff in the upper
middle
and lower reaches of the Yellow River all decreased from 1969 to 2018. The average annual reduction rates at the Lanzhou
Huayuankou
and Lijin stations were 51
355
and 413 million m3/a
respectively. ② In the last 50 years
the greatest alteration of natural runoff and observed runoff occurred during 1986 and 1990. Combined with previous studies and important water events of the Yellow River
the runoff alteration in 1986 may have been related to the implementation of soil and water conservation measures since 1984 as well as the construction of Longyangxia Reservoir in 1986. The runoff alteration in 1990 may have been due to the surge of water consumption in the 1980s and 1990s in addition to the underlying surface water variation of the basin. ③ The difference between the natural and observed runoff gradually increased from the upper reach to the lower reach
which was generally consistent with the increased average water consumption over the past 15 years. In addition
the annual average observed runoff only accounted for 42% of natural runoff at Lijin Station. The two regions with the highest water consumption were the lower part of Huayuankou and the area between Lanzhou and Toudaoguai
reaching 1.06×1010 m3 and 1.04×1010 m3
respectively.[Conclusion] The main reason for the large difference between the natural and observed runoff in the area below Lanzhou station was the water consumption associated with human activities
especially for farmland irrigation. Therefore
it is necessary to promote the development of water-saving agriculture in the Yellow River basin and to reasonably allocate water consumption.
Wu Jingwen, Zheng Haiyan, Xi Yang. SWAT-based runoff simulation and runoff responses to climate change in the headwaters of the Yellow River, China[J]. Atmosphere, 2019,10(9):509.
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