Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China; Academy of Disaster Reduction and Emergency Management, Ministry of Emergency Management and Ministry of Education, Beijing Normal University, Beijing 100875, China.
Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China; Academy of Disaster Reduction and Emergency Management, Ministry of Emergency Management and Ministry of Education, Beijing Normal University, Beijing 100875, China.
Sci Total Environ. 2019 Nov 25;693:133550. doi: 10.1016/j.scitotenv.2019.07.356. Epub 2019 Jul 23.
Climate change may considerably influence flash floods by increasing extreme precipitation. Coastal regions in eastern and southern China may experience especially negative effects because of the frequent occurrence of tropical cyclones (TCs). This study presented a hazard assessment framework for TCs-induced flash floods under climate change scenarios and assessed future inundations in Hadahe River basin, which is in northeastern China. From 1965 to 2014, there were twenty-four TCs ranging from severe tropical storm to super typhoon over Hadahe River basin in twenty years. General Circulation Models (GCMs) are too coarse to depict the impact of TCs on extreme precipitation; therefore, hourly precipitation data from two gauges and the tracks of TCs were used to assess the impact of TCs. An extreme precipitation event on 3-4 August 2012 and the same 600-year future probabilistic extreme rainfall were utilized to investigate the impact of climate change. Daily precipitation data from eight climate models from the NEX-GDDP dataset during 1965-2005 and 2050-2099 represented historical and future simulation conditions, respectively. The hydrologic model HEC-HMS was integrated with the hydraulic model FLO-2D to simulate discharges and inundations of past and future TCs episodes. The results showed that flooded area is projected to increase by 6.6% and 7.8% for inundation depth between 1.0 and 3.0 m under RCP 4.5 and RCP 8.5 scenarios, respectively. For inundation depth over 3.0 m, flooded area is projected to increase by 17.6% and 22.0%. Relative change of flash flood extent increases as inundation depth increases, indicating that climate change is likely to increase the risk of flash floods. Additional adaptation measures are needed to make the Hadahe River basin and other similar coastal basins more resilient. The results also indicated that considering the impact of TCs produces a more reliable assessment of future flash floods in coastal regions.
气候变化可能会通过增加极端降水而极大地影响山洪暴发。由于热带气旋(TCs)频繁发生,中国东部和南部沿海地区可能会受到特别不利的影响。本研究提出了一个在气候变化情景下针对 TCs 引发的山洪暴发的危害评估框架,并评估了中国东北部哈德河盆地的未来洪水情况。从 1965 年到 2014 年,在过去的二十年中,哈德河盆地共发生了二十四次从强热带风暴到超级台风的 TCs。一般环流模式(GCMs)过于粗糙,无法描述 TCs 对极端降水的影响;因此,使用两个雨量计的小时降水数据和 TCs 的轨迹来评估 TCs 的影响。利用 2012 年 8 月 3 日至 4 日的一次极端降水事件和相同的 600 年未来概率极端降雨来研究气候变化的影响。利用来自 NEX-GDDP 数据集的八个气候模型在 1965 年至 2005 年和 2050 年至 2099 年期间的日降水数据分别代表历史和未来的模拟条件。水文模型 HEC-HMS 与水力模型 FLO-2D 集成,以模拟过去和未来 TCs 事件的流量和洪水淹没情况。结果表明,在 RCP4.5 和 RCP8.5 情景下,淹没深度在 1.0-3.0m 之间的洪水面积预计分别增加 6.6%和 7.8%;淹没深度超过 3.0m 的洪水面积预计将增加 17.6%和 22.0%。随着洪水深度的增加,山洪暴发范围的相对变化增加,表明气候变化可能会增加山洪暴发的风险。需要采取更多的适应措施,使哈德河盆地和其他类似沿海流域更具弹性。研究结果还表明,考虑 TCs 的影响可以更可靠地评估沿海地区未来的山洪暴发。