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Combination of rainfall thresholds and susceptibility maps in regional-scale landslide warning systems

机译:区域尺度滑坡预警系统中降雨阈值和敏感性图的组合

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In this work, we propose a methodology to couple rainfall thresholds and susceptibility maps in the frame-work of regional scale landslide warning systems. While statistical rainfall thresholds are used to accomplish a temporal forecasting with very coarse spatial resolution, landslide susceptibility maps provide a static spatial information about the probability of landslide occurrence. If the susceptibility map is subdivided in a number of susceptibility classes that equals the number of possible alert levels featured in the threshold system, it is possible to establish a correspondence where the higher the alert level, the lower the degree of susceptibility that could be actually interested by landslides. Using past rainfall and landslide data, we tested this approach in two test sites, corresponding to the Emilia Romagna region ad to an experimental area within Tuscany region, Italy. Results show that the proposed approach would have contributed to define a more accurate location for up to 93% of the landslides correctly forecasted by the regional warning system. Civil protection agencies could use the proposed approach during the alert phases to better define the areas that are possibly going to be affected by landslides. The proposed approach is easy to implement and could be applied to any case of study in which rainfall thresholds and susceptibility maps have been previously defined.
机译:在这项工作中,我们提出了一种在区域尺度滑坡预警系统的框架中耦合降雨阈值和敏感性图的方法。虽然使用统计降雨阈值来完成具有非常粗糙的空间分辨率的时间预测,但是滑坡敏感性图提供了有关滑坡发生概率的静态空间信息。如果将磁化率图细分为与阈值系统中可能的警报级别数目相等的多个磁化率类别,则可以建立对应关系,其中警报级别越高,实际可能的磁化度越低对滑坡感兴趣。利用过去的降雨和滑坡数据,我们在两个测试地点测试了该方法,这两个地点分别对应于意大利的托斯卡纳地区的艾米利亚·罗马涅地区和艾米利亚·罗马涅地区。结果表明,所提出的方法将有助于为区域预警系统正确预测的多达93%的滑坡定义更准确的位置。民事保护机构可以在预警阶段使用提议的方法来更好地定义可能会受到山体滑坡影响的区域。所提出的方法易于实施,并且可以应用于之前已经定义了降雨阈值和磁化率图的任何研究案例。

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