Abstract
Predicting rainfall-induced landslides hinges on the quality of the rainfall product. Satellite rainfall estimates or rainfall reanalyses aid in studying landslide occurrences especially in ungauged areas, or in the absence of ground-based rainfall radars. Quality of these rainfall estimates is critical; hence, they are commonly crosschecked with their ground-based counterparts. Beyond their temporal precision compared to ground-based observations, we investigate whether these rainfall estimates are adequate for hindcasting landslides, which particularly requires accurate representation of spatial variability of rainfall. We developed a logistic regression model to hindcast rainfall-induced landslides in two sites in Japan. The model contains only a few topographic and geologic predictors to leave room for different rainfall products to improve the model as additional predictors. By changing the input rainfall product, we compared GPM IMERG and ERA5 rainfall estimates with ground radar–based rainfall data. Our findings emphasize that there is a lot of room for improvement of spatiotemporal prediction of landslides, as shown by a strong performance increase of the models with the benchmark radar data attaining 95% diagnostic performance accuracy. Yet, this improvement is not met by global rainfall products which still face challenges in reliably capturing spatiotemporal patterns of precipitation events.
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 3119-3133 |
| Seitenumfang | 15 |
| Fachzeitschrift | Landslides |
| Jahrgang | 18 |
| Ausgabenummer | 9 |
| DOIs | |
| Publikationsstatus | Veröffentlicht - 19 Sept. 2021 |
| Extern publiziert | Ja |
Fördermittel
Open Access funding enabled and organized by Projekt DEAL. This project is supported by the Federal Ministry of Education and Research of Germany (BMBF) within the project CLIENT II – CaTeNA (FKZ 03G0878A). Part of the research activity is funded by the Disaster Prevention Research Institute of Kyoto University (Long-Term Research Visit 2019L-01) and supported by the German Academic Exchange Service (DAAD) within the Co-PREPARE project of the German-Indian Partnerships Support Program (DIP, Project No.: 57553291). We thank Geological Survey of Japan for providing freely the Seamless Digital Geological Map of Japan (1:200000) (https://gbank.gsj.jp/seamless) and the ALOS for 30 m DEM (https://www.eorc.jaxa.jp/ALOS/en/aw3d30/index.htm). The GPM IMERG data were provided by the NASA/Goddard Space Flight Center (http://dx.doi.org/10.5067/GPM/IMERG/3B-HH/06). We further acknowledge the Copernicus Climate Change Service for providing the ERA5 rainfall reanalyses (http://dx.doi.org/10.24381/cds.adbb2d47), and Japan Meteorological Agency (JMA) for the rainfall radar data (http://www.data.jma.go.jp/add/suishin/cgi-bin/catalogue/make_product_page.cgi?id=KaisekiU). Although we computed the Soil Water Index (SWI) in this study, it is also available via JMA (https://www.data.jma.go.jp/add/suishin/cgi-bin/catalogue/make_product_page.cgi?id=Dojouryo). We highly appreciate Sebastian von Specht and Masumi Yamada for critically commenting on our results. We are sincerely grateful to Kevin Fleming for proof reading the early versions of the paper. In memory of Prof. Hiroshi Fukuoka (Sassa et al. 2018).
ÖFOS 2012
- 105902 Naturgefahren
- 105206 Meteorologie
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