Articles | Volume 15, issue 7
https://doi.org/10.5194/nhess-15-1617-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhess-15-1617-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Jul 2015
Research article |
| 24 Jul 2015
Hydrologic sensitivity of flood runoff and inundation: 2011 Thailand floods in the Chao Phraya River basin
T. Sayama
CORRESPONDING AUTHOR
International Centre for Water Hazard and Risk Management, Public Works Research Institute, Tsukuba, Japan
now at: Disaster Prevention Research Institute, Kyoto University, Uji, Japan
Y. Tatebe
International Centre for Water Hazard and Risk Management, Public Works Research Institute, Tsukuba, Japan
now at: CTI Engineering, Co. Ltd., Tokyo, Japan
Y. Iwami
International Centre for Water Hazard and Risk Management, Public Works Research Institute, Tsukuba, Japan
S. Tanaka
International Centre for Water Hazard and Risk Management, Public Works Research Institute, Tsukuba, Japan
now at: Disaster Prevention Research Institute, Kyoto University, Uji, Japan
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64 citations as recorded by crossref.
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- Application of Backpack-Mounted Mobile Mapping System and Rainfall–Runoff–Inundation Model for Flash Flood Analysis T. Sayama et al. 10.3390/w11050963
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Saved (final revised paper)
Latest update: 21 Nov 2024
Short summary
In 2011 the Chao Phraya River basin received about 1400mm rainfall, which was 1.2 times more than past large floods in 1995 and 2006.
The long-term rainfall-runoff-inundation simulation and its water balance analysis revealed high elasticity in the flood inundation volume (4.2%).
1.2 times more rainfall might result in 1.6 times more flood inundation volume in 2011.
The high sensitivity of inundation should be well recognized for a better understanding of the flood hazard characteristics.
In 2011 the Chao Phraya River basin received about 1400mm rainfall, which was 1.2 times more...
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