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A GIS method for assessment of rock slide tsunami hazard in Norwegian lakes and reservoirs

机译:挪威湖泊和水库滑坡海啸灾害评估的GIS方法

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An evaluation of rock slide tsunami hazard is applied to all Norwegian lakes larger than 0.1 km(2) based on their topographical setting. The analysis results in a topographic rock slide potential score that indicates the relative hazard in each lake. Even though the score value each lake receives should be interpreted with caution, the distribution of score values shows that we are able to make a clear distinction between lakes with a high vs. lakes with a low hazard. The results also show a clustering of threatened lakes in parts of Western Norway as well as some locations in Northern Norway. This makes the results useful as a tool for focusing further studies on regions or specific lakes that received high scores. The results also show how the method may be used for more detailed analysis of a given lake (or fjord). Maps can be produced that may serve as a guide when carrying out field campaigns or when designing scenarios for numerical simulations of tsunamis in the lake. It should be emphasised that the rock slide potential reported for each lake is based on the topographical setting alone and hence, does not represent the actual probability of rock slides into the lakes. For a given area, more detailed investigations of the geology, triggering factors and frequency of previous rock slide events should be carried out before definite statements about the actual hazard can be made.
机译:根据其地形设置,对所有大于0.1 km(2)的挪威湖泊均进行了岩屑海啸危险性评估。通过分析得出地形滑坡的潜在得分,该得分表明了每个湖泊的相对危害。尽管应该谨慎地解释每个湖泊收到的得分值,但是得分值的分布表明,我们能够对危险程度较高的湖泊与危险程度较低的湖泊进行明确区分。结果还显示挪威西部部分地区以及挪威北部某些地区的受威胁湖泊聚集在一起。这使结果成为有用的工具,可用于对获得高分的地区或特定湖泊进行进一步研究。结果还显示了如何将该方法用于给定湖泊(或峡湾)的更详细分析。可以制作地图,这些地图可以在进行野战或设计湖泊海啸数值模拟方案时用作指导。应该强调的是,每个湖泊报告的岩石滑坡潜力仅基于地形设置,因此,并不代表岩石滑坡进入湖泊的实际概率。对于给定的区域,应在对实际危险做出明确陈述之前,对地质,触发因素和以前的岩石滑动事件的频率进行更详细的研究。

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