Derivation of voellmy model parameters for landslide runout based on co-seismic rock avalanche inventory.
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| Title: | Derivation of voellmy model parameters for landslide runout based on co-seismic rock avalanche inventory. |
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| Authors: | Huang, Jhih-Rou1 (AUTHOR) jhihrou_huang@berkeley.edu, Zekkos, Dimitrios1 (AUTHOR) zekkos@berkeley.edu |
| Source: | Landslides. Jun2026, Vol. 23 Issue 6, p1529-1544. 16p. |
| Subject Terms: | *Rockslides, *Landslides, *Landslide prediction, *Earthquakes, *Friction measurements |
| Abstract: | Runout analyses are a key component of landslide risk assessment and mitigation. Natural disasters provide the opportunity to observe and document the runout of landslides, and these observations can be used to calibrate simple empirical or mechanistic runout models by providing valuable site or region-specific insights. A simple mechanical model that is based on the Voellmy friction law as incorporated in Rapid Mass Movement Simulation Debris Flow (RAMMS-DF), is regressed against hundreds of mapped rock avalanches that were triggered by the Mw 6.5 Lefkada earthquake on November 17, 2015, with the intent to statistically calibrate the two model parameters against numerous observations of landslide runout. It is found that the dry-Coulomb friction (μ) governs the performance of the simulation, whereas the results are less sensitive to viscous-turbulent friction (ξ), especially for large values of ξ. The mode and standard deviation of the dry-Coulomb friction (μ) are found to be 0.9 and 0.28, and the mode and standard deviation of the viscous-turbulent friction (ξ) are 3000 m/s2 and 3314 m/s2. The accuracy of the RAMMS-DF simulation positively correlates with landslide source area, height, and 3D travel distance. The model does not match smaller landslides well (with source areas < 4,000 m2), and in these cases, it systematically overestimates runout compared to field observations. [ABSTRACT FROM AUTHOR] |
| Database: | Energy & Power Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: enr DbLabel: Energy & Power Source An: 193627809 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Derivation of voellmy model parameters for landslide runout based on co-seismic rock avalanche inventory. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Huang%2C+Jhih-Rou%22">Huang, Jhih-Rou</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> jhihrou_huang@berkeley.edu</i><br /><searchLink fieldCode="AR" term="%22Zekkos%2C+Dimitrios%22">Zekkos, Dimitrios</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> zekkos@berkeley.edu</i> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Landslides%22">Landslides</searchLink>. Jun2026, Vol. 23 Issue 6, p1529-1544. 16p. – Name: Subject Label: Subject Terms Group: Su Data: *<searchLink fieldCode="DE" term="%22Rockslides%22">Rockslides</searchLink><br />*<searchLink fieldCode="DE" term="%22Landslides%22">Landslides</searchLink><br />*<searchLink fieldCode="DE" term="%22Landslide+prediction%22">Landslide prediction</searchLink><br />*<searchLink fieldCode="DE" term="%22Earthquakes%22">Earthquakes</searchLink><br />*<searchLink fieldCode="DE" term="%22Friction+measurements%22">Friction measurements</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Runout analyses are a key component of landslide risk assessment and mitigation. Natural disasters provide the opportunity to observe and document the runout of landslides, and these observations can be used to calibrate simple empirical or mechanistic runout models by providing valuable site or region-specific insights. A simple mechanical model that is based on the Voellmy friction law as incorporated in Rapid Mass Movement Simulation Debris Flow (RAMMS-DF), is regressed against hundreds of mapped rock avalanches that were triggered by the Mw 6.5 Lefkada earthquake on November 17, 2015, with the intent to statistically calibrate the two model parameters against numerous observations of landslide runout. It is found that the dry-Coulomb friction (μ) governs the performance of the simulation, whereas the results are less sensitive to viscous-turbulent friction (ξ), especially for large values of ξ. The mode and standard deviation of the dry-Coulomb friction (μ) are found to be 0.9 and 0.28, and the mode and standard deviation of the viscous-turbulent friction (ξ) are 3000 m/s2 and 3314 m/s2. The accuracy of the RAMMS-DF simulation positively correlates with landslide source area, height, and 3D travel distance. The model does not match smaller landslides well (with source areas < 4,000 m2), and in these cases, it systematically overestimates runout compared to field observations. [ABSTRACT FROM AUTHOR] |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1007/s10346-026-02736-7 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 16 StartPage: 1529 Subjects: – SubjectFull: Rockslides Type: general – SubjectFull: Landslides Type: general – SubjectFull: Landslide prediction Type: general – SubjectFull: Earthquakes Type: general – SubjectFull: Friction measurements Type: general Titles: – TitleFull: Derivation of voellmy model parameters for landslide runout based on co-seismic rock avalanche inventory. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Huang, Jhih-Rou – PersonEntity: Name: NameFull: Zekkos, Dimitrios IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 06 Text: Jun2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 1612510X Numbering: – Type: volume Value: 23 – Type: issue Value: 6 Titles: – TitleFull: Landslides Type: main |
| ResultId | 1 |