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Flood hazard assessment under climate change scenarios in the Yang River Basin, Thailand

机译:泰国阳河流域气候变化情景下的洪水灾害评估

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Climate change is expected to increase both the magnitude and frequency of extreme precipitation events, which may lead to more intense and frequent river flooding. This study aims to assess the flood hazard potential under climate change scenarios in Yang River Basin of Thailand. A physically-based distributed hydrological model, Block-wise use of TOPMODEL using Muskingum-Cunge flow routing (BTOPMC) and hydraulic model, HEC-RAS was used to simulate the floods under future climate scenarios. Future climate scenarios were constructed from the bias corrected outputs of three General Circulation Models (GCMs) for 2020s, 2050s and 2080s. Results show that basin will get warmer and wetter in future. Both the minimum and maximum temperature of the basin is projected to increase in future. Similarly average annual rainfall is also projected to increase in future, higher in near future and lower in far future. The extreme runoff pattern and synthetic inflow hydrographs for 25, 50 and 100year return flood were derived from an extreme flood of 2007 which were then fed into HEC-RAS model to generate the flood inundation maps in the basin. The intensity of annual floods is expected increase for both RCP 4.5 and 8.5 scenarios. Compared to the baseline period, an additional 60km 2 area of basin is projected to be flooded with the return period of 100years. The results of this study will be helpful to formulate adaptation strategies to offset the negative impacts of flooding on different land use activities in Yang River Basin.
机译:预计气候变化将增加极端降水事件的数量和频率,这可能导致更加强烈和频繁的河流洪水。这项研究旨在评估泰国杨河流域气候变化情景下的洪灾潜在风险。基于物理的分布式水文模型,使用Muskingum-Cunge流量路径(BTOPMC)和水力模型的TOPMODEL的逐块使用,HEC-RAS用于模拟未来气候情景下的洪水。未来气候情景是根据2020年代,2050年代和2080年代的三种通用环流模型(GCM)的偏差校正后的输出得出的。结果表明,未来盆地会变暖和变湿。预计该盆地的最低和最高温度都将在未来增加。同样,预计未来的年平均降雨量也将增加,在不久的将来会更高,在不久的将来会更低。 25年,50年和100年回洪的极端径流模式和合成流入水文图来自2007年的一次极端洪水,然后将其输入HEC-RAS模型以生成流域的洪水淹没图。对于RCP 4.5和8.5方案,预计每年的洪水强度都会增加。与基线期相比,预计将有60 km 2的额外流域被洪水淹没,回归期为100年。这项研究的结果将有助于制定适应策略,以抵消洪水对阳河流域不同土地利用活动的负面影响。

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