Abstract
The Ning-Meng reach of the Yellow River in China is located in a high-latitude area, and river freezes up and breaks up every year, leading to ice flood and disaster. Since the 1990s, due to the rising winter temperatures, river channel shrinkage and impacts of reservoir operation, the river ice regime of the Ning-Meng reach has changed. This paper investigated reservoir operation effect on river ice regime by eliminating the impact of climatic conditions, and the test method could be applied to other rivers, where similar anthropogenic impacts can be suspected to affect the river ice regime. The results show that compared to the statistics when there were no reservoirs, the duration of ice freezing days reduced 8–33 days, and the ice cover thickness was 16–25 cm thinner than that without reservoirs. The average number of ice flood incidents per year decreased from 11.61 to 3.25, and the number of disasters reduced from 1.69 to 1.41. Moreover, the changes induced by reservoirs joint operation may vastly exceed that by single reservoir operation. The smaller is the distance to the upstream reservoir, the more obvious is the impact from the reservoir.
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Acknowledgments
This research was supported by the Natural Science Foundation of China (51179148, 51179149) and Key Innovation Group of Science and Technology of Shaanxi (2012KCT-10). Sincere gratitude is extended to the editor and the anonymous reviewers for their professional comments and corrections.
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Chang, J., Wang, X., Li, Y. et al. Ice regime variation impacted by reservoir operation in the Ning-Meng reach of the Yellow River. Nat Hazards 80, 1015–1030 (2016). https://doi.org/10.1007/s11069-015-2010-5
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DOI: https://doi.org/10.1007/s11069-015-2010-5