Omar Cruz-Vázquez, Lucia Capra, Lorenzo Borselli, Norini Gianluca
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引用次数: 0
Abstract
El Chichón volcano, located in the southern part of Mexico, is one of the most active Mexican volcanoes. In 1982 it was the scene of the largest Plinian eruption recorded in Mexico during the last century. The volcano is in a climatic region with extreme rainfalls that accumulate more than 3,500 mm of precipitation per year and is frequently affected by hurricanes. The most recent climatic events were caused by Hurricane Eta in 2020 and tropical storm Karl in 2022, in addition to an atypical rainfall event in the same year that accumulated 339.9 mm of rain in 24 hours. During these episodes, hundreds of soil slips originated and transformed into inter-eruptive (e.g., secondary) lahars affecting several communities in the area.
In this work, we present a morpho-hydrological characterization of 33 catchments that drain from the volcano, including their geology and land use changes, to identify the factors promoting mass wasting processes. Moreover, rainfall frequency analysis was performed with data from six weather stations for the period 1987–2017, and precipitation scenarios with return periods of 5, 10, 20 and 80 years were defined. Based on these results, rainfall-runoff simulations using the FLO-2D code allowed us to obtain discharge curves for each catchment, which were used to simulate inter-eruptive lahars from the volcano slopes. We present the first hazard maps for inter-eruptive lahars based on the probability of occurrence and flow magnitude. These maps were subdivided into three scenarios: for 24 hours, 72 hours and an atypical event. The Ostuacán and Xochimilco villages are the most exposed inhabited areas with a total population of 4,000. These maps represent a new contribution to the volcanic hazard assessment of the El Chichón volcano and an essential instrument necessary to contribute to risk management.
El Chichón火山位于墨西哥南部,是墨西哥最活跃的火山之一。1982年,这里发生了上个世纪墨西哥有记录以来最大的普林尼火山喷发。这座火山所处的气候区降水极端,年降水量超过3500毫米,经常受到飓风的影响。最近的气候事件是由2020年的飓风埃塔和2022年的热带风暴卡尔造成的,此外,同一年还有一次非典型降雨事件,24小时内累计降雨量为339.9毫米。在这些事件中,数百次土壤滑动形成并转化为爆发间(例如,次生)火山泥流,影响了该地区的几个社区。在这项工作中,我们提出了33个从火山流出的集水区的形态水文特征,包括它们的地质和土地利用变化,以确定促进大规模浪费过程的因素。利用1987—2017年6个气象站数据进行降水频率分析,定义了回归期为5、10、20和80年的降水情景。基于这些结果,使用FLO-2D代码进行降雨径流模拟,使我们能够获得每个集水区的流量曲线,这些曲线用于模拟火山斜坡上的火山泥流。我们提出了第一个基于发生概率和流量大小的爆发间火山泥流的危险图。这些地图被细分为三个场景:24小时、72小时和非典型事件。Ostuacán村和Xochimilco村是受灾最严重的居民区,总人口为4000人。这些地图是对El Chichón火山的火山危险性评估的一项新贡献,也是对风险管理作出贡献的必要工具。
期刊介绍:
Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with:
the interactions between surface processes and landforms and landscapes;
that lead to physical, chemical and biological changes; and which in turn create;
current landscapes and the geological record of past landscapes.
Its focus is core to both physical geographical and geological communities, and also the wider geosciences