Abstract
Abstract. Landslide forecasting and early warning has a long tradition in landslide
research and is primarily carried out based on empirical and statistical
approaches, e.g., landslide-triggering rainfall thresholds. In the last
decade, flood forecasting started the operational mode of so-called ensemble
prediction systems following the success of the use of ensembles for weather
forecasting. These probabilistic approaches acknowledge the presence of
unavoidable variability and uncertainty when larger areas are considered and
explicitly introduce them into the model results. Now that highly detailed
numerical weather predictions and high-performance computing are becoming more
common, physically based landslide forecasting for larger areas is becoming
feasible, and the landslide research community could benefit from the
experiences that have been reported from flood forecasting using ensemble
predictions. This paper reviews and summarizes concepts of ensemble
prediction in hydrology and discusses how these could facilitate improved
landslide forecasting. In addition, a prototype landslide forecasting system
utilizing the physically based TRIGRS (Transient Rainfall Infiltration and Grid-Based Regional Slope-Stability) model is presented to highlight how
such forecasting systems could be implemented. The paper concludes with a
discussion of challenges related to parameter variability and uncertainty,
calibration and validation, and computational concerns.
Subject
General Earth and Planetary Sciences
Cited by
35 articles.
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