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Recent catastrophic debris flows in Chile: Geological hazard, climatic relationships and human response

机译:智利最近的灾难性泥石流:地质灾害,气候关系和人类应对

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摘要

Debris flows are an important type of geological hazard in Chile, affecting cities, towns and rural areas throughout the country despite the variation in climate regimes. In this summary paper, recent debris flows in the cities of Antofagasta and Santiago, in northern and central Chile, and in a rural area near Lake Ranco in central-southern Chile in 1991, 1993 and 2004, respectively, are reviewed. Triggering factors for flow occurrence are identified and different approaches to debris flow hazard assessment and the effects of debris flows on people and the environment are discussed. Furthermore, the relationships between debris flow occurrence and climatic anomalies such as El Nino episodes are analysed. A clear pattern of debris flow generation associated with El Nino events is found for Antofagasta and Santiago. The risk related to debris flows in Chile is of increasing importance because of the continuous expansion of cities to hazardous areas such as alluvial fans. The results show that hazard assessment based on several factors is essential for the implementation of proper prevention and mitigation measures for future debris flow events in the country.
机译:在智利,泥石流是一种重要的地质灾害类型,尽管气候条件有所不同,但仍影响着全国的城市,城镇和农村地区。在本摘要文件中,分别回顾了1991年,1993年和2004年智利北部和中部的安托法加斯塔和圣地亚哥市以及智利中南部的兰科湖附近的农村地区的近期泥石流。确定了流量发生的触发因素,并讨论了泥石流危险性评估的不同方法以及泥石流对人和环境的影响。此外,分析了泥石流发生与气候异常(如厄尔尼诺现象)之间的关系。在安托法加斯塔和圣地亚哥发现了与厄尔尼诺事件有关的泥石流产生的清晰模式。由于城市不断扩展到冲积扇等危险区域,与智利泥石流有关的风险变得越来越重要。结果表明,基于多种因素的危害评估对于为该国未来的泥石流事件实施适当的预防和缓解措施至关重要。

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