A model for spatially and temporally distributed shallow landslide initiation by rainfall infiltration
By: W. Z. Savage, J. W. Godt, and R.L. Baum
Edited by: Rickenmann D.Chen C.L.
Links
- The Publications Warehouse does not have links to digital versions of this publication at this time
- Download citation as: RIS | Dublin Core
Abstract
We describe a model for regional initiation of shallow landslides based on an approximate analytic solution to Richards equation combined with an infinite-slope calculation. The model applied over digital topography computes pressure heads and factors of safety as functions of depth for geographic information system (GIS) grid cells at any time during and after rainfall events. An example is presented that simulates the progressive development of shallow landslides on steep slopes during a rainfall event. This example shows how this modeling provides insights into transient rainfall-caused processes that trigger shallow slope instability and consequent regionally distributed debris-flow events. Specifically, we infer that the spatial pattern of instability is primarily controlled by topography, while intensity and duration of rainfall, and the subsequent pore-pressure responses control the temporal pattern of instability. ?? 2003 Millpress.
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | A model for spatially and temporally distributed shallow landslide initiation by rainfall infiltration |
| Volume | 1 |
| Year Published | 2003 |
| Language | English |
| Larger Work Title | International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment, Proceedings |
| First page | 179 |
| Last page | 187 |
| Conference Title | 3rd International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment |
| Conference Location | Davos |
| Conference Date | 10 September 2003 through 12 September 2003 |
| Google Analytic Metrics | Metrics page |