2019 年 10 月 22 日西班牙东北部加泰罗尼亚灾难性山洪的水文气象控制和社会反应

A. Amengual, Romualdo Romero, M. Llasat, A. Hermoso, M. Llasat-Botija
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摘要

摘要2019 年 10 月 22 日,西班牙东北部加泰罗尼亚的弗朗科利河流域遭遇强降水事件,导致灾难性山洪暴发,造成 6 人死亡。很少有研究全面探讨特大山洪暴发时的物理和人文因素及其相互关系。本研究通过考察所有这些因素之间的相互关系,为填补这一知识空白迈出了一步。水文气象因素的研究采用了新的基于三角区的区域大气模型、雷达降水估算、洪水后的实地观测和测量仪观测以及运动学局部过剩模型。通过研究流域动态与预警响应时间之间的关系,以及通过事后的公民科学活动量化山洪暴发过程中的人类行为,对社会层面进行了评估。研究结果表明,一股持续的东南气流带来了低层水汽,并在该地区形成了对流不稳定性,而当地的地形则有助于引发深层湿润对流。一列对流促进了西北部集水区上游的强降水,降水量大且持续时间长。盆地的反应受到非常干燥的初始土壤水分条件的极大影响。在长时间降雨之后,一阵急剧的降水导致了特大山洪暴发。溪流流量的快速突然增加影响了较小的空间尺度,留给有效实施保护措施的时间有限。机构组织--保护--预防的循环在通常由气象尺度而非水文尺度主导的时空尺度上展开。尽管公民科学活动表明,预警能够有效地传达到生活在受影响最严重地区的居民,但相当一部分受访者表示缺乏足够的信息或不熟悉预期的含义。此外,大多数受访者认为生命或财产没有受到任何重大威胁。鉴于这些结果,本研究确定了今后改进类似自然灾害社会防备的潜在领域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrometeorological controls of and social response to the 22 October 2019 catastrophic flash flood in Catalonia, north-eastern Spain
Abstract. On 22 October 2019, the Francolí River basin in Catalonia, north-eastern Spain, experienced a heavy precipitation event that resulted in a catastrophic flash flood, causing six fatalities. Few studies comprehensively address both the physical and human dimensions and their interrelations during extreme flash flooding. This research takes a step forward towards filling this gap in knowledge by examining the alignment among all these factors. The hydrometeorological factors are investigated using the new Triangle-based Regional Atmospheric Model, radar-derived precipitation estimates, post-flood field and gauge observations, and the Kinematic Local Excess Model. The social dimension is assessed by examining the relationship between catchment dynamics and warning response times and by quantifying human behaviour during the course of the flash flood through a post-event citizen science campaign. Results reveal that a persistent south-easterly airflow brought low-level moisture and established convective instability in the region, while local orography was instrumental to triggering deep moist convection. A convective train promoted intense, copious, and prolonged precipitation over the north-western catchment headwaters. Basin response was significantly modulated by the very dry initial soil moisture conditions. After the long-lasting rainfall, an acute burst of precipitation resulted in extreme flash flooding. Fast and abrupt increases in streamflow affect small spatial scales and leave limited time for the effective implementation of protective measures. The institutional organization–protection–prevention cycle unfolded at the spatial and temporal scales typically dominated by the meteorological rather than hydrological scales. Although the citizen science campaign reveals the effectiveness of the warnings in reaching the population living in the most affected areas, a significant proportion of the respondents expressed a lack of adequate information or were unfamiliar with the intended meaning. In addition, a majority of the interviewees did not perceive any significant threat to life or property. In view of these results, this study identifies potential areas for improving social preparedness for similar natural hazards in the future.
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