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.

Highlights

  • Landslide prediction at the regional scale is a hot topic within the scientific community as the time-varying aspects of landslide susceptibilities, hazards, and even risks are crucial for emergency response planning and protecting public safety (Baum et al, 2010; Glade and Crozier, 2015)

  • 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

  • We provide a review on how probabilistic modeling methods and in particular ensemble predictions are applied for hydrological forecasts and how these deal with uncertainties

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Summary

Introduction

Landslide prediction at the regional scale is a hot topic within the scientific community as the time-varying aspects of landslide susceptibilities, hazards, and even risks are crucial for emergency response planning and protecting public safety (Baum et al, 2010; Glade and Crozier, 2015). The number of landslides is assumed to increase due to global change (Crozier, 2010; Gariano et al, 2017; PapathomaKöhle and Glade, 2013). This calls for increased efforts for the development of early warning procedures with the aim of issuing timely warnings of an upcoming hazardous event to temporarily reduce the exposure of vulnerable persons or infrastructure (Thiebes and Glade, 2016). Warnings can be considered calls for the public to take protective action, and the timescale of a warning depends on the associated weather event (Stensrud et al, 2009)

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