RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin

Climatic variations caused by the excessive emission of greenhouse gases are likely to change the patterns of precipitation, runoff processes, and water storage of river basins. Various studies have been conducted based on precipitation outputs of the global scale climatic models under different emi...

Full description

Bibliographic Details
Main Authors: Edangodage Duminda Pradeep Perera, Takahiro Sayama, Jun Magome, Akira Hasegawa, Yoichi Iwami
Format: Article
Language:English
Published: MDPI AG 2017-11-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/4/4/55
id doaj-a94c99c2c81a4efcafa75d534f4953d9
record_format Article
spelling doaj-a94c99c2c81a4efcafa75d534f4953d92020-11-25T01:42:22ZengMDPI AGHydrology2306-53382017-11-01445510.3390/hydrology4040055hydrology4040055RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River BasinEdangodage Duminda Pradeep Perera0Takahiro Sayama1Jun Magome2Akira Hasegawa3Yoichi Iwami4United Nations University–Institute forWater, Environment and Health, Hamilton, ON L8P 0A1, CanadaDisaster Prevention Research Institute, Kyoto University, Kyoto 611-0011, JapanInternational Research Centre for River Basin Environment, University of Yamanashi, Kofu 400-8511, JapanInternational Centre for Water Hazard and Risk Management, Public Works Research Institute, Tsukuba, Ibaraki 302-8516, JapanNagasaki Prefectural Civil Engineering Department, Nagasaki 850-8570, JapanClimatic variations caused by the excessive emission of greenhouse gases are likely to change the patterns of precipitation, runoff processes, and water storage of river basins. Various studies have been conducted based on precipitation outputs of the global scale climatic models under different emission scenarios. However, there is a limitation in regional- and local-scale hydrological analysis on extreme floods with the combined application of high-resolution atmospheric general circulation models’ (AGCM) outputs and physically-based hydrological models (PBHM). This study has taken an effort to overcome that limitation in hydrological analysis. The present and future precipitation, river runoff, and inundation distributions for the Lower Mekong Basin (LMB) were analyzed to understand hydrological changes in the LMB under the RCP8.5 scenario. The downstream area beyond the Kratie gauging station, located in the Cambodia and Vietnam flood plains was considered as the LMB in this study. The bias-corrected precipitation outputs of the Japan Meteorological Research Institute atmospheric general circulation model (MRI-AGCM3.2S) with 20 km horizontal resolution were utilized as the precipitation inputs for basin-scale hydrological simulations. The present climate (1979–2003) was represented by the AMIP-type simulations while the future (2075–2099) climatic conditions were obtained based on the RCP8.5 greenhouse gas scenario. The entire hydrological system of the Mekong basin was modelled by the block-wise TOPMODEL (BTOP) hydrological model with 20 km resolution, while the LMB area was modelled by the rainfall-runoff-inundation (RRI) model with 2 km resolution, specifically to analyze floods under the aforementioned climatic conditions. The comparison of present and future river runoffs, inundation distributions and inundation volume changes were the outcomes of the study, which can be supportive information for the LMB flood management, water policy, and water resources development.https://www.mdpi.com/2306-5338/4/4/55climate changeflood hazardshigh-resolution AGCMinundation analysisLower Mekong river basin
collection DOAJ
language English
format Article
sources DOAJ
author Edangodage Duminda Pradeep Perera
Takahiro Sayama
Jun Magome
Akira Hasegawa
Yoichi Iwami
spellingShingle Edangodage Duminda Pradeep Perera
Takahiro Sayama
Jun Magome
Akira Hasegawa
Yoichi Iwami
RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
Hydrology
climate change
flood hazards
high-resolution AGCM
inundation analysis
Lower Mekong river basin
author_facet Edangodage Duminda Pradeep Perera
Takahiro Sayama
Jun Magome
Akira Hasegawa
Yoichi Iwami
author_sort Edangodage Duminda Pradeep Perera
title RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
title_short RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
title_full RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
title_fullStr RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
title_full_unstemmed RCP8.5-Based Future Flood Hazard Analysis for the Lower Mekong River Basin
title_sort rcp8.5-based future flood hazard analysis for the lower mekong river basin
publisher MDPI AG
series Hydrology
issn 2306-5338
publishDate 2017-11-01
description Climatic variations caused by the excessive emission of greenhouse gases are likely to change the patterns of precipitation, runoff processes, and water storage of river basins. Various studies have been conducted based on precipitation outputs of the global scale climatic models under different emission scenarios. However, there is a limitation in regional- and local-scale hydrological analysis on extreme floods with the combined application of high-resolution atmospheric general circulation models’ (AGCM) outputs and physically-based hydrological models (PBHM). This study has taken an effort to overcome that limitation in hydrological analysis. The present and future precipitation, river runoff, and inundation distributions for the Lower Mekong Basin (LMB) were analyzed to understand hydrological changes in the LMB under the RCP8.5 scenario. The downstream area beyond the Kratie gauging station, located in the Cambodia and Vietnam flood plains was considered as the LMB in this study. The bias-corrected precipitation outputs of the Japan Meteorological Research Institute atmospheric general circulation model (MRI-AGCM3.2S) with 20 km horizontal resolution were utilized as the precipitation inputs for basin-scale hydrological simulations. The present climate (1979–2003) was represented by the AMIP-type simulations while the future (2075–2099) climatic conditions were obtained based on the RCP8.5 greenhouse gas scenario. The entire hydrological system of the Mekong basin was modelled by the block-wise TOPMODEL (BTOP) hydrological model with 20 km resolution, while the LMB area was modelled by the rainfall-runoff-inundation (RRI) model with 2 km resolution, specifically to analyze floods under the aforementioned climatic conditions. The comparison of present and future river runoffs, inundation distributions and inundation volume changes were the outcomes of the study, which can be supportive information for the LMB flood management, water policy, and water resources development.
topic climate change
flood hazards
high-resolution AGCM
inundation analysis
Lower Mekong river basin
url https://www.mdpi.com/2306-5338/4/4/55
work_keys_str_mv AT edangodagedumindapradeepperera rcp85basedfuturefloodhazardanalysisforthelowermekongriverbasin
AT takahirosayama rcp85basedfuturefloodhazardanalysisforthelowermekongriverbasin
AT junmagome rcp85basedfuturefloodhazardanalysisforthelowermekongriverbasin
AT akirahasegawa rcp85basedfuturefloodhazardanalysisforthelowermekongriverbasin
AT yoichiiwami rcp85basedfuturefloodhazardanalysisforthelowermekongriverbasin
_version_ 1725036959387090944