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dc.contributor.authorLo, W-Cen_US
dc.contributor.authorLin, B-Sen_US
dc.contributor.authorHo, H-Cen_US
dc.contributor.authorKeck, J.en_US
dc.contributor.authorYin, H-Yen_US
dc.contributor.authorShan, H-Yen_US
dc.date.accessioned2014-12-08T15:28:55Z-
dc.date.available2014-12-08T15:28:55Z-
dc.date.issued2012en_US
dc.identifier.issn1561-8633en_US
dc.identifier.urihttp://hdl.handle.net/11536/20899-
dc.identifier.urihttp://dx.doi.org/10.5194/nhess-12-3407-2012en_US
dc.description.abstractThe occurrence of typhoon Herb in 1996 caused massive landslides in the Shenmu area of Taiwan. Many people died and stream and river beds were covered by meters of debris. Debris flows almost always take place in the Shenmu area during the flood season, especially in the catchment areas around Tsushui river and Aiyuzih river. Anthropogenic and natural factors that cause debris flow occurrences are complex and numerous. The precise conditions of initiation are difficult to be identified, but three factors are generally considered to be the most important ones, i.e. rainfall characteristics, geologic conditions and topography. This study proposes a simple and feasible process that combines remote sensing technology and multi-stage high-precision DTMs from aerial orthoimages and airborne LiDAR with field surveys to establish a connection between three major occurrence factors that trigger debris flows in the Shenmu area.en_US
dc.language.isoen_USen_US
dc.titleA simple and feasible process for using multi-stage high-precision DTMs, field surveys and rainfall data to study debris flow occurrence factors of Shenmu area, Taiwanen_US
dc.typeArticleen_US
dc.identifier.doi10.5194/nhess-12-3407-2012en_US
dc.identifier.journalNATURAL HAZARDS AND EARTH SYSTEM SCIENCESen_US
dc.citation.volume12en_US
dc.citation.issue11en_US
dc.citation.spage3407en_US
dc.citation.epage3419en_US
dc.contributor.department土木工程學系zh_TW
dc.contributor.departmentDepartment of Civil Engineeringen_US
dc.identifier.wosnumberWOS:000311804900018-
dc.citation.woscount1-
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