Where did the Yellow River flood occur?

1953 floods in some areas of the lower Yellow River

1954 flood disasters in the main stream and tributaries of the middle and lower reaches of the Yellow River, Weihe River, Fenhe River and Xiliao River Basin in Northeast China.

1957 floods in parts of the middle and lower reaches of the Yellow River.

1958, the middle and lower reaches of the Yellow River flooded, and the main stream and tributaries of the Sanhua section of the Yellow River were submerged by the three rivers of Yi, Luo and Qin. The measured peak flow at Huayuankou of the main stream is 22,300 m3/s, and the flood is a great threat to the lower reaches of the Yellow River, and the traffic across the Beijing-Guangzhou railway bridge of the Yellow River is interrupted 14 days. There are 1708 flooded villages in the Yellow River beach area and Dongping Lake area, with 200,000 hectares of flooded farmland and 300,000 houses.

There was a flood in the upper reaches of the Yellow River.

1977 floods occurred in the middle and lower reaches of Yanhe River, Beiluo River and Jinghe River, and the measured peak flow at Yanhe Gangu Station was 9050m3/s, with the return period exceeding 100. The flood peak discharge at Tongguan Station of the Yellow River is 1.54 million m3/s, which is the largest since the actual measurement record.

198 1 September, the maximum flood occurred in the upper reaches of the Yellow River, with the maximum discharge of 5450m3/s at Tangnaihai Station and the peak discharge of 5600m3/s at Lanzhou Station. The floods in Shaanxi and Gansu provinces are more serious.

1982, the third flood occurred in Sanhua section of the main stream of the Yellow River since 1949, with the peak flow of Huayuankou 15300m3/s, the lower reaches of the beach were generally covered, and the farmland was affected173,000 hm2.

In the 22nd year of the Republic of China (1933), in August of 10, a flood peak of 2000m3/s occurred at Shaanxi Station of the Yellow River, covering more than 5 counties in Wenxian, Wuzhi, Changyuan, Lanfeng and Kaocheng, Henan Province, and inundating 30 counties in 4 provinces at that time, with the affected area of 6592 km2. The property loss was 270 million yuan (silver dollars at that time). Cao Xian, Juye, Dingtao and Shan counties were drowned. The seventh dike of the Yellow River around Xuzhou has been opened for more than ten miles. The water potential of journey to the south makes Pu, Fan, Shouzhang and Yanggu counties become Zeguo; All the way south, the invasion of Anhui Boxian and Yang Guo. Fortunately, the current is a little slow, and the disaster is not huge. Changyuan County, Hebei Province, was the hardest hit, starting from the east bank levee and Pangzhuang, Li Ji, Suji and Chengzhuang in the east and reaching the counties of Cyclobalanopsis, Zhangtun and Xiangru in the west, with a width of 60 miles and an area of more than 40 miles. The affected area accounts for 9/ 10 of the total area of the county. 1933 during July and August, the yellow river basin suffered severe floods, among which Hebei, Shandong and Henan provinces suffered the most, with the affected area exceeding 1 10,000 square kilometers, the affected population exceeding 3 million and the property loss exceeding 200 million yuan. After the disaster, the National Government set up the Yellow River Flood Relief Committee to carry out emergency rescue and disaster relief and health and epidemic prevention. Although the disaster relief activities had a sound organization and system, the failure of flood relief not only aggravated the agricultural panic in China at that time, but also reflected the weakness of the Nanjing National Government in disaster relief. In August, 2003, there was a flood in the middle reaches of the Yellow River, and the peak flow of Shaanxi County Station was 22,000 cubic meters per second. The flood caused more than 50 breaches on the north and south banks of the lower Yellow River, flooded 30 counties in Henan, Shandong, Hebei and Jiangsu provinces, and killed 1.27 million people.