Department of Civil and Environmental Engineering, Western University, London, Ontario N6A3K7, Canada; Department of Water Resources Development and Management, Indian Institute of Technology Roorkee, Roorkee, Uttarakhand 247667, India.
Department of Water Resources Development and Management, Indian Institute of Technology Roorkee, Roorkee, Uttarakhand 247667, India.
Sci Total Environ. 2021 Oct 20;792:148323. doi: 10.1016/j.scitotenv.2021.148323. Epub 2021 Jun 8.
With the recent Coupled Model Intercomparison Project Phase 6 (CMIP6), water experts and flood modellers are curious to explore the efficacy of the new and upgraded climate models in representing flood inundation dynamics and how they will be impacted in the future by climate change. In this study, for the first time, we consider the latest group of General Circulation Models (GCMs) from CMIP6 to examine the probable changes in floodplain regimes over Canada. A set of 17 GCMs from Shared Socioeconomic Pathways (SSPs) 4.5 (medium forcing) and 8.5 (high end forcing) common to historical (1980 to 2019), near-future (2021 to 2060), and far-future (2061 to 2100) time-periods are selected. A comprehensive framework consisting of hydrodynamic flood modelling, and statistical experiments are put forward to derive high-resolution Canada-wide floodplain maps for 100 and 200-yr return periods. The changes in floodplain regimes for the future periods are analyzed over drainage basin scale in terms of (i) changes in flood inundation extents, (ii) changes in flood hazards (high and very-high classes), and (iii) changes in flood frequency. Our results show a significant rise (>30%) in flood inundation extents in the future periods; particularly intense over western and eastern regions. The flood hazards are expected to cover ~16% more geographical area of Canada. We also find that large areas in northern and western Canada and a few spots in the eastern parts of Canada will be getting flooded more frequently compared to the historical period. The observations derived from this study are vital for enhancing flood preparedness, optimal land-use planning, and refurbishing both structural and non-structural flood control options for improved resilience. The study instills new knowledge on revamping the existing flood management approaches and adaptation strategies for future protection.
利用最近的耦合模式比较计划第六阶段(CMIP6),水专家和洪水建模师们渴望探索新的和升级的气候模型在代表洪水泛滥动态方面的效果,以及它们在未来将如何受到气候变化的影响。在这项研究中,我们首次考虑了来自 CMIP6 的最新一组通用环流模型(GCM),以研究加拿大洪泛区制度可能发生的变化。选择了来自共享社会经济途径(SSP)4.5(中等强迫)和 8.5(高强迫)的 17 个 GCM,这些 GCM 共同涵盖了历史时期(1980 年至 1999 年)、近期(2021 年至 2060 年)和远期(2061 年至 2100 年)。提出了一个包含水动力洪水建模和统计实验的综合框架,以推导出 100 年和 200 年重现期的加拿大全范围洪泛区地图。未来时期洪泛区制度的变化在流域尺度上进行了分析,包括:(i)洪水泛滥范围的变化,(ii)洪水危害(高和极高类别)的变化,以及(iii)洪水频率的变化。我们的结果表明,未来时期的洪水泛滥范围显著上升(>30%);特别是在西部和东部地区更为强烈。洪水危害预计将覆盖加拿大更多的地理区域(约 16%)。我们还发现,加拿大北部和西部的大片地区以及加拿大东部的少数地区将比历史时期更频繁地发生洪水。这项研究得出的观测结果对于提高洪水准备、优化土地利用规划以及修复结构和非结构洪水控制措施以提高恢复力至关重要。该研究为改进现有的洪水管理方法和适应未来保护的策略提供了新的知识。