Regional-scale flood impacts on a small mountainous catchment in Thailand under a changing climate

Sawitree Rojpratak, Seree Supharatid
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Abstract

Extreme rainfall and flooding are common during the summer monsoon season in Thailand. In this study, we utilized Robust Empirical Quantile Mapping (RQUANT) to correct the bias in precipitation, and total runoff data obtained from the latest Couple Model Intercomparison Project phase 6 (CMIP6) for the upper Lam Takong river basin. Five different methods were employed to estimate the river discharge and four estimations based on Budyko functions. Our analysis revealed that the ‘Total runoff’ method yielded the most accurate representation of the observed discharge. Impacts of change in land use are examined in terms of compound roughness. The Multi-Model Ensemble (MME) precipitation under medium-emission (SSP2-4.5) and high-emission (SSP5-8.5) scenarios is projected to increase by 5.74 and 10.91%, respectively. Correspondingly, the discharges are expected to increase by 4.57 and 11.05% for the far-future periods. In general, the Flo-2D model satisfactorily simulated the water level in the main channel but it underestimated small inundation depth (<0.5 m) across the floodplain. Comparing inundation maps among different scenarios and timelines, changes in the inundation area were relatively small (0.05%), especially when compared to changes in floodplain storage (6.85%) due to the mountainous nature of the river basin.

气候变化对泰国一个小型山区集水区的区域性洪水影响
泰国夏季季风季节经常出现极端降雨和洪水。在这项研究中,我们利用鲁棒经验量子绘图法(RQUANT)来纠正降水量的偏差,以及从最新的夫妇模式相互比较项目第 6 阶段(CMIP6)中获得的林德孔上游流域的总径流数据。我们采用了五种不同的方法来估算河流径流量,其中四种估算方法基于布迪科函数。我们的分析表明,"总径流量 "方法最准确地反映了观测到的排水量。从复合粗糙度的角度考察了土地利用变化的影响。在中排放(SSP2-4.5)和高排放(SSP5-8.5)情景下,多模型集合(MME)降水量预计将分别增加 5.74% 和 10.91%。相应地,远期的排水量预计将增加 4.57% 和 11.05%。总体而言,Flo-2D 模型对主河道水位的模拟令人满意,但低估了整个洪泛区的小淹没深度(0.5 米)。比较不同方案和不同时间段的淹没图,淹没面积的变化相对较小(0.05%),特别是与洪泛区蓄水量的变化(6.85%)相比,这是因为该流域多山。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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