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JDR Vol.15 No.7 pp. 1025-1039
(2020)
doi: 10.20965/jdr.2020.p1025

Paper:

Assessing Flood Risk of the Chao Phraya River Basin Based on Statistical Rainfall Analysis

Shakti P. C.*1,†, Mamoru Miyamoto*2, Ryohei Misumi*1, Yousuke Nakamura*3, Anurak Sriariyawat*4, Supattra Visessri*4,*5, and Daiki Kakinuma*2

*1National Research Institute for Earth Science and Disaster Resilience (NIED)
3-1 Tennodai, Tsukuba, Ibaraki 305-0006, Japan

Corresponding author

*2International Centre for Water Hazard and Risk Management under the auspices of UNESCO (ICHARM),
Public Works Research Institute (PWRI), Ibaraki, Japan

*3Mitsui Consultants Co., Ltd., Tokyo, Japan

*4Department of Water Resources Engineering, Faculty of Engineering, Chulalongkorn University, Bangkok, Thailand

*5Disaster and Risk Management Information Systems Research Group, Faculty of Engineering, Chulalongkorn University, Bangkok, Thailand

Received:
June 25, 2020
Accepted:
September 7, 2020
Published:
December 1, 2020
Keywords:
probability distribution, return period of rainfall, design hyetograph, flood inundation, Chao Phraya Basin
Abstract

The Chao Phraya River Basin is one of the largest in Asia and is highly vulnerable to water-related disasters. Based on rainfall gauge data over 36 years (1981–2016), a frequency analysis was performed for this basin to understand and evaluate its overall flood risk; daily rainfall measurements of 119 rain gauge stations within the basin were considered. Four common probability distributions, i.e., Log-Normal (LOG), Gumbel type-I (GUM), Pearson type-III (PE3), and Log-Pearson type-III (LP3) distributions, were used to calculate the return period of rainfall at each station and at the basin-scale level. Results of each distribution were compared with the graphical Gringorten method to analyze their performance; GUM was found to be the best-fitted distribution among the four. Thereafter, design hyetographs were developed by integrating the return period of rainfall based on three adopted methods at basin and subbasin scales; each method had its pros and cons for hydrological applications. Finally, utilizing a Rainfall-Runoff-Inundation (RRI) model, we estimated the possible flood inundation extent and depth, which was outlined over the Chao Phraya River Basin using the design hyetographs with different return periods. This study can help enhance disaster resilience at industrial complexes in Thailand for sustainable growth.

Cite this article as:
Shakti P. C., M. Miyamoto, R. Misumi, Y. Nakamura, A. Sriariyawat, S. Visessri, and D. Kakinuma, “Assessing Flood Risk of the Chao Phraya River Basin Based on Statistical Rainfall Analysis,” J. Disaster Res., Vol.15 No.7, pp. 1025-1039, 2020.
Data files:
References
  1. [1] D. Gu, “Exposure and vulnerability to natural disasters for world’s cities,” United Nations, Department of Economics and Social Affairs, Population Division, Technical Paper, No.4, pp. 1-43, 2019.
  2. [2] Centre for Research on the Epidemiology of Disasters (CRED) and United Nations International Strategy for Disaster Reduction (UNISDR), “The human cost of weather-related disasters 1995–2015,” pp. 1-30, 2015, https://www.unisdr.org/2015/docs/climatechange/COP21_WeatherDisastersReport_2015_FINAL.pdf [accessed June 5, 2020]
  3. [3] H. Baba, T. Watanabe, K. Miyata, and H. Matsumoto, “Area business continuity management, a new approach to sustainable local economy,” J. Disaster Res., Vol.10, No.2, pp. 204-209, doi: 10.20965/jdr.2015.p0204, 2015.
  4. [4] Science and Technology Research Partnership for Sustainable Development (SATREPS), “Regional Resilience Enhancement through Establishment of Area-BCM at Industry Complexes in Thailand,” https://www.jst.go.jp/global/english/kadai/h2908_thailand.html [accessed June 1, 2020]
  5. [5] F. Fujibe, “Long-term changes in precipitation in Japan,” J. Disaster Res., Vol.3, No.1, pp. 51-60, doi: 10.20965/jdr.2008.p0051, 2008.
  6. [6] M. A. Alam, K. Emura, C. Farnham, and J. Yuan, “Best-fit probability distributions and return periods for maximum monthly rainfall in Bangladesh,” Climate, Vol.6, No.1, Article 9, doi: 10.3390/cli6010009, 2018.
  7. [7] S. Zenkoji, S. Oda, T. Tebakari, and B. Archevarahuprok, “Spatial characteristics of flooded areas in the Mun and Chi River Basins in Northeastern Thailand,” J. Disaster Res., Vol.14, No.9, pp. 1337-1345, doi: 10.20965/jdr.2019.p1337, 2019.
  8. [8] F. A. Huff and J. C. Neill, “Comparison of several methods for rainfall frequency analysis,” J. Geophys. Res., Vol.64, No.5, pp. 541-547, doi: 10.1029/JZ064i005p00541, 1959.
  9. [9] V. T. Chow, D.R. Maidment, and L. W. Mays, “Applied Hydrology,” McGraw-Hill, 1988.
  10. [10] M. T. Amin, M. Rizwan, and A. A. Alazba, “A best-fit probability distribution for the estimation of rainfall in northern regions of Pakistan,” Open Life Sci., Vol.11, pp. 432-440, doi: 10.1515/biol-2016-0057, 2016.
  11. [11] Z. Li, Z. J. Li, W. Zhao, and Y. Wang, “Probability modeling of precipitation extremes over two river basins in northwest of china,” Adv. Meteorol., Article ID.374127, doi: 10.1155/2015/374127, 2015.
  12. [12] A. Wang, N. Qu, Y. Chen, Q. Li, and S. Gu, “A 60-minute design rainstorm for the urban area of Yangpu District, Shanghai, China,” Water, Vol.10, No.3, Article 312, doi: 10.3390/w10030312, 2018.
  13. [13] S. Wongsa, “2011 Thailand Flood,” J. Disaster Res., Vol.8, No.3, pp. 380-385, doi: 10.20965/jdr.2013.p0380, 2013.
  14. [14] Y. Hagiwara, D. Kuribayashi, and H. Sawano, “Enhancement of flood countermeasures of Japanese-affiliated firms based on the lessons learned from the 2011 Thai flood,” J. Disaster Res., Vol.11, No.6, pp. 1176-1189, doi: 10.20965/jdr.2016.p1176, 2016.
  15. [15] D. Komori, C. Mateo, A. Saya, S. Nakamura, M. Kiguchi, P. Klinkhachorn, T. Sukhapunnaphan, A. Champathong, K. Takeya, and T. Oki, “Application of the probability evaluation for the seasonal reservoir operation on flood mitigation and water supply in the Chao Phraya River Watershed, Thailand,” J. Disaster Res., Vol.8, No.3, pp. 432-446, doi: 10.20965/jdr.2013.p0432, 2013.
  16. [16] S. Wichakul, Y. Tachikawa, M. Shiiba, and K. Yorozu, “Development of a flow routing model including inundation effect for the extreme flood in the Chao Phraya River Basin, Thailand 2011,” J. Disaster Res., Vol.8, No.3, pp. 415-423, doi: 10.20965/jdr.2013.p0415, 2013.
  17. [17] H. Takebayashi, K. Toda, H. Nakagawa, and H. Zhang, “Field and interview surveys of the flood of 2011, Thailand,” J. Disaster Res., Vol.8, No.3, pp. 386-396, doi: 10.20965/jdr.2013.p0386, 2013.
  18. [18] S. Kotsuki and K. Tanaka, “Impacts of mid-rainy season rainfall on runoff into the Chao Phraya River, Thailand,” J. Disaster Res., Vol.8, No.3, pp. 397-405, doi: 10.20965/jdr.2013.p0397, 2013.
  19. [19] T. Sayama, Y. Tatebe, and S. Tanaka, “An emergency response-type rainfall-runoff-inundation simulation for 2011 Thailand floods,” J. Flood Risk Management, Vol.10, No.1, pp. 65-78, doi: 10.1111/jfr3.12147, 2017.
  20. [20] B. B. Shrestha, E. D. P. Perera, S. Kudo et al., “Assessing flood disaster impacts in agriculture under climate change in the river basins of Southeast Asia,” Nat. Hazards, Vol.97, No.1, pp. 157-192, doi: 10.1007/s11069-019-03632-1, 2019.
  21. [21] J. V. Campenhout, G. Houbrechts, A. Peeters, and F. Petit, “Return period of characteristic discharges from the comparison between partial duration and annual series, application to the Walloon Rivers (Belgium),” Water, Vol.12, No.3, Article 792, doi: 10.3390/w12030792, 2020.
  22. [22] World Meteorological Organization (WMO), “Guide to Climatological Practices,” WMO No.100, 1983.
  23. [23] S. P. C., T. Nakatani, and R. Misumi, “Hydrological simulation of small river basins in Northern Kyushu, Japan, during the extreme rainfall event of July 5–6, 2017,” J. Disaster Res., Vol.13, No.2, pp. 396-409, doi: 10.20965/jdr.2018.p0396, 2018.
  24. [24] S. P. C., T. Nakatani, and R. Misumi, “Analysis of flood inundation in ungauged mountainous river basins: a case study of an extreme rain event on 5–6 July 2017 in Northern Kyushu, Japan,” J. Disaster Res., Vol.13, No.5, pp. 860-872, doi: 10.20965/jdr.2018.p0860, 2018.
  25. [25] S. P. C., H. Kamimera, and R. Misumi, “Inundation analysis of the Oda River Basin in Japan during the flood event of 6–7 July 2018 utilizing local and global hydrographic data,” Water, Vol.12, No.4, Article 1005, doi: 10.3390/w12041005, 2020.
  26. [26] T. Sayama, G. Ozawa, T. Kawakami, S. Nabesaka, and K. Fukami, “Rainfall-runoff-inundation analysis of the 2010 Pakistan flood in the Kabul River basin,” Hydrological Science J., Vol.57, No.2, pp. 298-312, doi: 10.1080/02626667.2011.644245, 2012.
  27. [27] A. Sriariyawat, K. Pakoksung, T. Sayama, S. Tanaka, and S. Koontanakulvong, “Approach to estimate the flood damage in Sukhothai Province using flood simulation,” J. Disaster Res., Vol.8, No.3, pp. 406-414, doi: 10.20965/jdr.2013.p0406, 2013.
  28. [28] S. P. C. and H. Kamimera, “Flooding in Oda River Basin during torrential rainfall event in July 2018,” Eng. J., Vol.23, No.6, pp. 477-485, doi: 10.4186/ej.2019.23.6.477, 2019.
  29. [29] S. P. C., T. Nakatani, and R. Misumi, “The role of the spatial distribution of radar rainfall on hydrological modeling for an urbanized river basin in Japan,” Water, Vol.11, No.8, Article 1703, doi: 10.3390/w11081703, 2019.
  30. [30] Z. Li, F. Brissette, and J. Chen, “Finding the most appropriate precipitation probability distribution for stochastic weather generation and hydrological modelling in Nordic watersheds,” Hydrological Processes, Vol.27, No.25, pp. 3718-3729, doi: 10.1002/hyp.9499, 2013.
  31. [31] J. Yuan, K. Emura, C. Farnham, and M. A. Alam, “Frequency analysis of annual maximum hourly precipitation and determination of best fit probability distribution for regions in Japan,” Urban Clim., Vol.24, pp. 276-286, doi: 10.1016/j.uclim.2017.07.008, 2018.
  32. [32] Y. Wakazuki, “New distribution functions for hourly and daily precipitation intensities during the snowless season in Japan,” J. Meteor. Soc. Japan, Vol.89, No.1, pp. 29-45, doi: 10.2151/jmsj.2011-103, 2011.
  33. [33] S. S. Eslamian and H. Feizi, “Maximum monthly rainfall analysis using L-moments for an Arid region in Isfahan Province, Iran,” J. Appl. Meteorol. Climatol., Vol.46, No.4, pp. 494-503, doi: 10.1175/JAM2465.1, 2007.
  34. [34] S. P. C., N. Shrestha, and P. Gurung, “Step wise multi-criteria performance evaluation of rainfall-runoff models using WETSPRO,” J. of Hydrology and Meteorology, Vol.7, No.1, pp. 18-29, doi: 10.3126/jhm.v7i1.5613, 2010.
  35. [35] S. P. C., R. Misumi, T. Nakatani, K. Iwanami, M. Maki, T. Maesaka, and K. Hirano, “Accuracy of quantitative precipitation estimation using operational weather radars: a case study of heavy rainfall on 9–10 September 2015 in the East Kanto Region, Japan,” J. Disaster Res., Vol.11, No.5, pp. 1003-1016, doi: 10.20965/jdr.2016.p1003, 2016.
  36. [36] S. P. C., K. Hirano, and S. Iizuka, “Flood inundation mapping of the Hitachi region in the Kuji River Basin, Japan, during the October 11–13, 2019 extreme rain event,” J. Disaster Res., Vol.15, No.6, pp. 712-725, doi: 10.20965/jdr.2020.p0712, 2020.

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