Abstract
Due to the effects of continual strong rainfall, 4 floods are generated in partial area of upper and middle reaches of Weihe, the largest branch in Yellow River, from Aug. 26 to Sep. 22 in 2003. The biggest flood peak of Huaxian station, which is 3570 m{sup 3}/s, occurred 11:00 in Sep. 1. It is the 33 rd among all historical biggest flood peaks, but the stage, 342.76 m, is the 1 st. During the evolution process of the flood, because of the effects of flood plain, inverse of branch flood, levee breach of partial branch etc. the largest cut down of flood peak of Lintong and Huaxian is 53.1 %, and the longest travel time is 52.3 h. Both are 1 st in history. The evolution characteristics of the flood and the most reasons of large cut down and long travel time are analyzed in this paper.(Author)
Jiang, Xinhui;
Huo, Shiqing;
Hu, Yuebin;
E-mail:xinhuijiang@163 net, Suqin Xu
[1]
- Hydrology Bureau, YRCC, Henan, Zhengzhou, 450004 (CHINA)
Citation Formats
Jiang, Xinhui, Huo, Shiqing, Hu, Yuebin, and E-mail:xinhuijiang@163 net, Suqin Xu.
Analysis of characteristic of flood evolution in Weihe middle and lower reaches in 2003.
Macedonia, The Former Yugoslav Republic of: N. p.,
2004.
Web.
Jiang, Xinhui, Huo, Shiqing, Hu, Yuebin, & E-mail:xinhuijiang@163 net, Suqin Xu.
Analysis of characteristic of flood evolution in Weihe middle and lower reaches in 2003.
Macedonia, The Former Yugoslav Republic of.
Jiang, Xinhui, Huo, Shiqing, Hu, Yuebin, and E-mail:xinhuijiang@163 net, Suqin Xu.
2004.
"Analysis of characteristic of flood evolution in Weihe middle and lower reaches in 2003."
Macedonia, The Former Yugoslav Republic of.
@misc{etde_20619592,
title = {Analysis of characteristic of flood evolution in Weihe middle and lower reaches in 2003}
author = {Jiang, Xinhui, Huo, Shiqing, Hu, Yuebin, and E-mail:xinhuijiang@163 net, Suqin Xu}
abstractNote = {Due to the effects of continual strong rainfall, 4 floods are generated in partial area of upper and middle reaches of Weihe, the largest branch in Yellow River, from Aug. 26 to Sep. 22 in 2003. The biggest flood peak of Huaxian station, which is 3570 m{sup 3}/s, occurred 11:00 in Sep. 1. It is the 33 rd among all historical biggest flood peaks, but the stage, 342.76 m, is the 1 st. During the evolution process of the flood, because of the effects of flood plain, inverse of branch flood, levee breach of partial branch etc. the largest cut down of flood peak of Lintong and Huaxian is 53.1 %, and the longest travel time is 52.3 h. Both are 1 st in history. The evolution characteristics of the flood and the most reasons of large cut down and long travel time are analyzed in this paper.(Author)}
place = {Macedonia, The Former Yugoslav Republic of}
year = {2004}
month = {Jul}
}
title = {Analysis of characteristic of flood evolution in Weihe middle and lower reaches in 2003}
author = {Jiang, Xinhui, Huo, Shiqing, Hu, Yuebin, and E-mail:xinhuijiang@163 net, Suqin Xu}
abstractNote = {Due to the effects of continual strong rainfall, 4 floods are generated in partial area of upper and middle reaches of Weihe, the largest branch in Yellow River, from Aug. 26 to Sep. 22 in 2003. The biggest flood peak of Huaxian station, which is 3570 m{sup 3}/s, occurred 11:00 in Sep. 1. It is the 33 rd among all historical biggest flood peaks, but the stage, 342.76 m, is the 1 st. During the evolution process of the flood, because of the effects of flood plain, inverse of branch flood, levee breach of partial branch etc. the largest cut down of flood peak of Lintong and Huaxian is 53.1 %, and the longest travel time is 52.3 h. Both are 1 st in history. The evolution characteristics of the flood and the most reasons of large cut down and long travel time are analyzed in this paper.(Author)}
place = {Macedonia, The Former Yugoslav Republic of}
year = {2004}
month = {Jul}
}