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Offshore Landslide Hazard Curves From Mapped Landslide Size Distributions

机译:来自映射滑坡尺寸分布的海上山体滑坡危险曲线

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摘要

We present a method to calculate landslide hazard curves along offshore margins based on size distributions of submarine landslides. The method utilizes 10 different continental margins that were mapped by high-resolution multibeam sonar with landslide scar areas measured by a consistent Geographic Information System procedure. Statistical tests of several different probability distribution models indicate that the lognormal model is most appropriate for these siliciclastic environments, consistent with an earlier study of the U.S. Atlantic margin (Chaytor et al., 2009, ). Parameter estimation is performed using the maximum likelihood technique, and confidence intervals are determined using likelihood profiles. Pairwise comparison of size distributions for the 10 margins indicates that the U.S. Atlantic and Queen Charlotte margins are different than most other margins. These margins represent end-members, with the U.S. Atlantic margin having the highest mean scar area and the Queen Charlotte margin the lowest. We demonstrate that empirical, offshore landslide hazard curves can be developed from the landslide size distributions, if the duration of mapped landslide activity is known. This study indicates that the shape parameter of the size distribution is similar among all 10 margins, and thus, the shape of the hazard curves is also similar. Significant differences in hazard curves among the margins are therefore related to differences in mean sizes and, potentially, differences in the duration of landslide activity.
机译:我们提出了一种方法来计算基于潜艇滑坡尺寸分布的海上边距来计算滑坡危险曲线。该方法利用了通过一致地理信息系统程序测量的高分辨率多滨声纳用高分辨率多沟声纳映射的10种不同的大陆边缘。若干不同概率分布模型的统计测试表明,Lognormal模型最适合于这些硅质型环境,与早期的美国大西洋边缘的研究一致(ChaYtor等,2009,)。使用最大似然技术执行参数估计,并且使用似然轮廓确定置信区间。对10个边缘的大小分布的成对比较表明美国大西洋和女王夏洛特利润率与大多数其他利润不同。这些边缘代表了最终成员,与美国大西洋边缘有最高的平均疤痕区域和女王夏洛特率最低。我们证明了实证,如果已知映射滑坡活动的持续时间,则可以从滑坡尺寸分布中开发经验,海上滑坡危害曲线。该研究表明,所有10个边缘的尺寸分布的形状参数相似,因此,危险曲线的形状也是相似的。因此,边缘之间的危险曲线的显着差异与平均尺寸的差异有关,并且可能是山体滑坡活动持续时间的差异。

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