论文标题
气候不断变化的山洪泛滥的时空聚类(中国,1950- 2015年)
Space-time clustering of flash floods in a changing climate (China, 1950-2015)
论文作者
论文摘要
在山洪灾害的空间和时间上的持久性 - 导致经济或生命损失或两者兼而有之的山洪是对遇到水文风险的区域的诊断度量。可以通过聚类分析来评估持久性的概念,并在此进行分析,以分析中国山洪灾害的国家清单发生在1950 - 2015年时期。具体来说,我们通过使用全球和局部方法研究了山洪及其聚类行为的时空模式分布:第一个基于Ripley的K功能,第二个基于扫描统计。结果,我们可以可视化聚合事件的模式,估计群集持续时间,并对它们随着时间的流逝进行假设,以及尊重降水趋势。由于数据集的空间(整个中国领土)和时间尺度(66年),我们能够捕获某些群集是否聚集在特定位置和时间上,而且它们的幅度是否倾向于增加或减小。总体而言,与该国其他地区相比,中国的东部地区遭受山洪的影响。被发现的集群表明,这些现象主要发生在7月至10月之间,这与中国的潮湿季节相吻合。检测到的簇的数量随时间增加,但是在最近的时期,相关持续时间大大减少。这可能表明改变了触发短期极端降雨事件的典型的机制。最后,被直接与降水及其极端实现有关的山洪泛滥,我们间接评估了扳机本身的大小是否在空间和时间上也有所不同,在气候变化的背景下使人们考虑了考虑。
The persistence over space and time of flash flood disasters -- flash floods that have caused either economical or life losses, or both -- is a diagnostic measure of areas subjected to hydrological risk. The concept of persistence can be assessed via clustering analyses, performed here to analyse the national inventory of flash floods disasters in China occurred in the period 1950-2015. Specifically, we investigated the spatio-temporal pattern distribution of the flash floods and their clustering behavior by using both global and local methods: the first, based on the Ripley's K-function, and the second on scan statistics. As a result, we could visualize patterns of aggregated events, estimate the cluster duration and make assumptions about their evolution over time, also with respect precipitations trend. Due to the large spatial (the whole Chinese territory) and temporal scale of the dataset (66 years), we were able to capture whether certain clusters gather in specific locations and times, but also whether their magnitude tends to increase or decrease. Overall, the eastern regions in China are much more subjected to flash floods compared to the rest of the country. Detected clusters revealed that these phenomena predominantly occur between July and October, a period coinciding with the wet season in China. The number of detected clusters increases with time, but the associated duration drastically decreases in the recent period. This may indicate a change towards triggering mechanisms which are typical of short-duration extreme rainfall events. Finally, being flash floods directly linked to precipitation and their extreme realization, we indirectly assessed whether the magnitude of the trigger itself has also varied through space and time, enabling considerations in the context of climatic changes.