Climate History Controls Future Landslide Hazard

与大风暴相关的强降水可能引发数千起山体滑坡和泥石流，危及生命，并对基础设施造成重大破坏。风暴频率和/或强度的变化是气候变化的预测结果（Rosenzweig等人，2007年），因此滑坡预测模型对于减轻这些影响至关重要。在土壤中发生的浅层滑坡破坏性特别大，因为它们往往会引发快速移动的泥石流。基于物理的浅层滑坡灾害模型通常根据现代水文、生态和土壤力学特性来估计滑坡（蒙哥马利和迪特里希，1994年;帕克等人，2001年）。这种方法的缺陷是它没有考虑到以前在一个集水区发生滑坡的“记忆”，在很短的时间内（<1000年），滑坡不太可能在同一地点发生两次。当滑坡的“记忆”被认为是，我们假设两种可能的影响，对未来的滑坡：（1）极端降雨将创建一个大的滑坡事件的可能性是依赖于最近发生在集水区的大型风暴的数量，和（2）风暴，启动1000的滑坡可能有一个共振的景观，导致滑坡集群的时间。当我们开始预测与气候变化相关的灾害时，考虑降水和景观共振的综合作用是一个紧迫的问题。拟议的研究将通过收集一个新的、大型的、千年规模的滑坡频率数据集，量化滑坡是否在时间上聚集。我们将分析滑坡频率使用放射性碳在75个空洞（当地沉积中心位于10米以上的渠道头）的基础上发现浅滑坡启动。这些数据与高分辨率LiDAR地形数据相结合，将推动创建一个独特的概率性滑坡灾害模型，该模型将根据最近的降水和以前风暴产生的潜在共振来估计滑坡灾害。我们新的滑坡数据集和滑坡灾害模型将显著提高我们在当前和未来气候情景下预测滑坡风险的能力。

The intense precipitation associated with large storms can initiate thousands of landslides and debris flows, endangering lives and cause significant damage to infrastructure. Changes to the frequency and/or intensity of storms is a predicted consequence of anthropogenically-driven climate change (Rosenzweig et al., 2007), thus predictive models of landsliding are essential for mitigating these effects. Shallow landslides that initiate in soil are particularly destructive as they often initiate rapidly moving debris flows. Physically-based shallow landslide hazard models usually estimate landsliding a function of modern hydrologic, ecologic, and soil mechanical properties (Montgomery and Dietrich, 1994; Pack et al., 2001). The flaw in this approach is that it does not account for the "memory" of previous landslides in a catchment, where landslides are unlikely to occur twice in the same location within the short window of time (<1000 years). When landslide "memory" is considered, we hypothesise two possible effects on future landsliding: (1) the likelihood that extreme rainfall will create a large landslide event is dependent on the number of large storms that have recently occurred in a catchment, and (2) storms that initiate a 1000's of landslides may have a resonance within a landscape that causes landslides to cluster in time. Accounting for the combined role of precipitation and landscape resonance is of immediate concern as we begin to make predict hazards associated with climate change. The proposed research will quantify whether landslides are clustered in time, through the collection of a novel, large, millennial-scale dataset of landslide frequency. We will analyse landslide frequency using radiocarbon found at the base of 75 hollows (local depocentres located 10's of metres above channel heads) where shallow landslides initiate. These data, in conjunction with high resolution LiDAR topographic data, will drive the creation of a unique, probabilistic, landslide hazard model that estimates landslide hazard based on both recent precipitation and the potential resonance imparted by previous storms. Our novel landslide dataset and landslide hazard model will significantly improve our ability to predict the risks posed by landslides in current and future climate scenarios.