Runoff Limit in the Yangtze River Estuary during Flood Season

被引:0
作者
Zhang, Weina [1 ]
Huang, Huiming [1 ]
Wang, Yigang [1 ]
机构
[1] Hohai Univ, Key Lab Coastal Disasters & Def, Minist Educ, Nanjing 210098, Jiangsu, Peoples R China
来源
2015 4TH INTERNATIONAL CONFERENCE ON ENERGY AND ENVIRONMENTAL PROTECTION (ICEEP 2015) | 2015年
关键词
Yangtze River Estuary; runoff limit; hammed tidal level; northeast expanding trend;
D O I
暂无
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The issue about extending area of Yangtze River Diluted Water is widely concerned. Through introducing the concept of runoff limit, a zone with tide level difference (hammed tide level) compared when there is an annual maximum runoff discharge with no runoff discharge in Datong is presented. Based on a 1-d hydraulic numerical model, water level boundary conditions in Xuliujing are acquired for 2-d tide current numerical model. Furtherly, 2-d model is verified by the hydrologic data observed in flood season. The results show the runoff limit is mostly limited within west of 123 degrees E, and there is a northeast expanding trend of the outer contour of runoff limit. Moreover, contributed to low flow diversion ratio of north branch, hammed tide level of tide wave in north branch is slightly influenced by runoff compared with south branch.
引用
收藏
页码:3937 / 3940
页数:4
相关论文
共 5 条
[1]  
[刘宝超 Liu Baochao], 2013, [海洋学报, Acta Oceanologica Sinica], V35, P25
[2]  
MAO Zhi-chang, 2001, MAR SCI, V25, P31
[3]  
[王建丰 Wang Jianfeng], 2012, [地球科学进展, Advance in Earth Sciences], V27, P194
[4]  
Wang Xin, 2013, Earth Science - Journal of China University of Geosciences, V38, P763, DOI 10.3799/dqkx.2013.074
[5]  
Zhu J., 1998, Haiyang Xuebao (in Chinese), V20, P13