Impacts of Mid-Rainy Season Rainfall on Runoff into the Chao Phraya River, Thailand

被引:15
作者
Kotsuki, Shunji [1 ]
Tanaka, Kenji [2 ]
机构
[1] Kyoto Univ, Grad Sch Engn, Nishikyo Ward, Kyoto 6158530, Japan
[2] Kyoto Univ, DPRI, Uji, Kyoto 6110011, Japan
基金
日本学术振兴会;
关键词
Chao Phraya River; flood; precipitation; soil water content; hydrological land surface model;
D O I
10.20965/jdr.2013.p0397
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In Chao Phraya River basin, the runoff at the middle basin (Nakhon Sawan station: C.2 point) is important for the prevention of lower basin floods. Through analyzing 1980 to 2011 runoff and rain gauge data and performing numerical calculations using a hydrological land surface model, this study will describe a condition that causes massive floods at the C.2 point. The main conclusions are the following: (1) In 2011, precipitation exceeding the average by about 40% caused naturalized runoff + 125% (+ 29 billion m(3)) that in an average year. The massive 2011 flood would have been difficult to prevent even if the operation of the Bhumi-bol Dam and Sirikit Dam had been appropriate. (2) In 1980, 1995, and 2006, precipitation exceeding the average by about 10% caused naturalized runoff exceeding that of the average year by 50 to 75%. The runoff rate in the Chao Phraya River basin is about 20%, and characteristically a minor increase in precipitation results in a considerable amount of runoff. (3) There are natural flood years, which have higher than average precipitation that causes massive floods, and there are non-natural flood years, which have high precipitation but no massive floods. In natural flood years, the precipitation in June, July, and August is higher than that in the average years, and the total water storage capacity is brought close to saturation in September. Due to this, in addition to base runoff, surface runoff increases. (4) The coefficient of the determination of observed runoff from August to October is 0.6481 for rainfall from June to August and 0.5276 for rainfall from August to October. Heavy rainfall in June, July and August has the effect of bringing the soil close to saturation, which is a necessary condition for massive flooding. Massive flooding results if this necessary condition is met and there is heavy rainfall in September and October. This finding is also supported by a high coefficient of determination of 0.7260 between rainfall in May, June, July, August, September, and October and naturalized runoff in August, September, and October.
引用
收藏
页码:397 / 405
页数:9
相关论文
共 15 条
[1]  
Fekete BM, 2004, J CLIMATE, V17, P294, DOI 10.1175/1520-0442(2004)017<0294:UIPATI>2.0.CO
[2]  
2
[3]  
Fekete S. F., 2013, GEOSCIENTIFIC MODEL, V5, P3573
[4]  
Hirabayashi Y, 2008, HYDROL RES LETT, V2, P36, DOI DOI 10.3178/HRL.2.36
[5]  
Homdee T., 2011, J JPN SOC CIV ENG SE, V67, DOI [10.2208/jscejhe.67.I_31, DOI 10.2208/JSCEJHE.67.I_31, DOI 10.2208/jscejhe.67.I_31]
[6]   River Discharge Projection under Climate Change in the Chao Phraya River Basin, Thailand, Using the MRI-GCM3.1S Dataset [J].
Hunukumbura, P. B. ;
Tachikawa, Yasuto .
JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2012, 90A :137-150
[7]   Characteristics of the 2011 Chao Phraya River flood in Central Thailand [J].
Komori, Daisuke ;
Nakamura, Shinichirou ;
Kiguchi, Masashi ;
Nishijima, Asako ;
Yamazaki, Dai ;
Suzuki, Satoshi ;
Kawasaki, Akiyuki ;
Oki, Kazuo ;
Oki, Taikan .
HYDROLOGICAL RESEARCH LETTERS, 2012, 6 :41-46
[8]  
Kotsuki S., HYDROLOGICAL R UNPUB
[9]   Hydrological impact of regional climate change in the Chao Phraya River Basin, Thailand [J].
Kure, Shuichi ;
Tebakari, Taichi .
HYDROLOGICAL RESEARCH LETTERS, 2012, 6 :53-58
[10]   The JRA-25 reanalysis [J].
Onogi, Kazutoshi ;
Tslttsui, Junichi ;
Koide, Hiroshi ;
Sakamoto, Masami ;
Kobayashi, Shinya ;
Hatsushika, Hiroaki ;
Matsumoto, Takanori ;
Yamazaki, Nobuo ;
Kaalhori, Hirotaka ;
Takahashi, Kiyotoshi ;
Kadokura, Shinji ;
Wada, Koji ;
Kato, Koji ;
Oyama, Ryo ;
Ose, Tomoaki ;
Mannoji, Nobutaka ;
Taira, Ryusuke .
JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2007, 85 (03) :369-432