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- W54167504 abstract "Every spring and winter ice floods often occur on the lower reach of the Yellow River, jamming up the river channel and raising the water level with the consequent overflowing of ice floods onto the floodplains. If the ice were to cause breaching of the dikes, a great disaster could occur. The Yellow River changed its course after the dike-breach at Tongwaxiang in 1855. During the following 54 years from 1883 to 1936, there were 21 years with dike-breaches occurring at 40 places along the lower reaches of the Yellow River during the ice-flood period. On average, dike-breaches took place once every other year. The menace of ice flooding has been somewhat reduced since the operation of Sanmenxia Reservoir in 1960. This paper deals with measures for ice flood prevention in the lower reaches of the Yellow River. It also gives a brief introduction to the characteristics of ice floods in the lower reaches and measures for ice-flood prevention currently practiced." @default.
- W54167504 created "2016-06-24" @default.
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- W54167504 date "1989-01-01" @default.
- W54167504 modified "2023-09-24" @default.
- W54167504 title "Ice Floods on the Lower Reach of the Yellow River and Measures for Ice Flood Prevention" @default.
- W54167504 doi "https://doi.org/10.1007/978-94-009-2450-5_30" @default.
- W54167504 hasPublicationYear "1989" @default.
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