Flood Response to Temporal Variation of Precipitation in Plain River Network Region in Taihu Lake Drainage Basin

HU Zi-chen, LIU Shu-guang, ZHONG Gui-hui, WEI Qian-kun

Journal of Changjiang River Scientific Research Institute ›› 2018, Vol. 35 ›› Issue (11) : 46-51.

PDF(5090 KB)
PDF(5090 KB)
Journal of Changjiang River Scientific Research Institute ›› 2018, Vol. 35 ›› Issue (11) : 46-51. DOI: 10.11988/ckyyb.20170570
FLOOD PREVENTION AND DISASTER REDUCTION

Flood Response to Temporal Variation of Precipitation in Plain River Network Region in Taihu Lake Drainage Basin

  • HU Zi-chen, LIU Shu-guang, ZHONG Gui-hui, WEI Qian-kun
Author information +
History +

Abstract

Flood and waterlogging disasters in plain river network region in recent years have brought about severe damage to people's lives and property safety. Rainfall is the key factor causing flood disasters in the region, of which the most typical ones are plum rain and typhoon rainstorm. The flood generating mechanism of plum rain and typhoon rainstorm varies because of different temporal distribution. In the aim of investigating the influence of rainfall's temporal variation on flood process, a 1D- and 2D-coupled hydrodynamic model of Wuchengxiyu hydraulic district of Taihu Lake drainage basin was built with MIKE 11 and MIKE 21. The model was calibrated and validated by several measured flood events. Numerical simulation of flood processes under different design conditions in the study area was conducted. The influences of magnitude, duration and temporal variation of rainfall on flood process were examined. Results suggest that the temporal distribution of rainfall has apparent influence on flood in plain river network. Rainfall of long duration is sensitive to the delay of rainfall peak, while rainfall of short duration is largely affected by the time variance coefficient. Meanwhile, rainfall amount has evident impact on both long-duration and short-duration rainfall.

Key words

Taihu Lake drainage basin / plain river network / temporal variation of rainfall / flood response / hydrodynamic simulation

Cite this article

Download Citations
HU Zi-chen, LIU Shu-guang, ZHONG Gui-hui, WEI Qian-kun. Flood Response to Temporal Variation of Precipitation in Plain River Network Region in Taihu Lake Drainage Basin[J]. Journal of Changjiang River Scientific Research Institute. 2018, 35(11): 46-51 https://doi.org/10.11988/ckyyb.20170570

References

[1] 许有鹏, 于瑞宏, 马宗伟. 长江中下游洪水灾害成因及洪水特征模拟分析[J]. 长江流域资源与环境, 2005, 14(5):638-643.
[2] 戴甦, 张怡. 太湖流域洪涝灾害特征及减灾措施[C]∥太湖高级论坛交流文集. 北京:中国水利学会,2004:81-86.
[3] 林木生, 陈兴伟, 陈莹. 晋江西溪流域洪水与暴雨时空分布特征的相关分析[J]. 资源科学, 2011, 33(12):2226-2231.
[4] 刘德地, 陈晓宏, 楼章华. 基于云模型的降雨时空分布特性分析[J]. 水利学报, 2009, 40(7):850-857.
[5] 崔腾科, 陈学林, 张文春,等. 阿尔金山东端北坡区域短历时降水及洪水时空分布规律分析[J]. 甘肃水利水电技术, 2016, 52(1):9-12.
[6] EMMANUEL I, ANDRIEU H, LEBLOIS E, et al. Influence of Rainfall Spatial Variability on Rainfall-runoff Modelling: Benefit of a Simulation Approach?[J]. Journal of Hydrology, 2015, 531:337-348.
[7] ARNAUD P, BOUVIER C, CISNEROS L, et al. Influence of Rainfall Spatial Variability on Flood Prediction[J]. Journal of Hydrology, 2002, 260(1/4):216-230.
[8] 张录军, 钱永甫. 长江流域汛期降水集中程度和洪涝关系研究[J]. 地球物理学报, 2004, 47(4):622-630.
[9] 胡彩虹, 王纪军, 詹发竹,等. 中小流域汛期降水时空分布集中程度与洪水关系研究[J]. 水文, 2009, 29(4):14-21.
[10] DHI. MIKE 11 A Modelling System for Rivers and Channels Reference Manual[M]. Hoersholm, Denmark: DHI, 2015.
[11] DHI. MIKE21 Flow Model-Hydrodynamic Module Scientific Documentation[M]. Hoersholm, Denmark: DHI, 2015.
[12] 韩超, 梅青, 刘曙光,等. 平原感潮河网水文水动力耦合模型的研究与应用[J]. 水动力学研究与进展, 2014, 29(6): 706-712.
[13] 程文辉, 王船海, 朱琰. 太湖流域模型[M]. 南京: 河海大学出版社, 2006.
[14] 唐敏. 上海城市化过程中的河网水系保护及相关环境效应研究[D]. 上海:华东师范大学, 2004.
[15] 江苏省水文总站. 江苏省暴雨洪水图集[M]. 南京: 江苏省水文总站,1984.
PDF(5090 KB)

Accesses

Citation

Detail

Sections
Recommended

/