Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 443572
Title Landslide model performance in a high resolution small-scale landscape
Author(s) Sy, V. De; Schoorl, J.M.; Keesstra, S.D.; Jones, K.E.; Claessens, L.F.G.
Source Geomorphology 190 (2013). - ISSN 0169-555X - p. 73 - 81.
DOI http://dx.doi.org/10.1016/j.geomorph.2013.02.012
Department(s) Soil Geography and Landscape
Soil Physics and Land Management
PE&RC
Publication type Refereed Article in a scientific journal
Publication year 2013
Keyword(s) physically-based model - soil redistribution - new-zealand - shallow landslides - sediment yield - dem resolution - stability - hazard - prediction
Abstract The frequency and severity of shallow landslides in New Zealand threatens life and property, both on- and off-site. The physically-based shallow landslide model LAPSUS-LS is tested for its performance in simulating shallow landslide locations induced by a high intensity rain event in a small-scale landscape. Furthermore, the effect of high resolution digital elevation models on the performance was tested. The performance of the model was optimised by calibrating different parameter values. A satisfactory result was achieved with a high resolution (1 m) DEM. Landslides, however, were generally predicted lower on the slope than mapped erosion scars. This discrepancy could be due to i) inaccuracies in the DEM or in other model input data such as soil strength properties; ii) relevant processes for this environmental context that are not included in the model; or iii) the limited validity of the infinite length assumption in the infinite slope stability model embedded in the LAPSUS-LS. The trade-off between a correct prediction of landslides versus stable cells becomes increasingly worse with coarser resolutions; and model performance decreases mainly due to altering slope characteristics. The optimal parameter combinations differ per resolution. In this environmental context the 1 m resolution topography resembles actual topography most closely and landslide locations are better distinguished from stable areas than for coarser resolutions. More gain in model performance could be achieved by adding landslide process complexities and parameter heterogeneity of the catchment.
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