Assessment of physical parameters impacts on debris flow modeling with RAMMS

The Rapid Mass Movement Simulation (RAMMS), requires input data such as DEM, the Voellmy-fluid friction coefficients, flow direction, and release information. To evaluate the uncertainties in RAMMS outputs using various input data, a real debris flow event was considered. After the calibration of the model, different scenarios were defined, which included different DEM cell sizes (1, 2, 3, 4, 5, 10, 15, and 20 m), different values of friction coefficients (the Dry-Coulomb type µ= [0.1, 0.2, 0.3]; the viscous-turbulent [Formula: see text]= [100, 200, 400, 800]), different directions of inflow (changes up to ± 50 degrees with a 10-degree interval), and active or inactive consideration of terrain curvature. The final results showed: (a) by increasing the DEM cell size, holding all other parameters constant, the accuracy of the model outputs (e.g. overall inundation area) reduced intensively which was up to 724% for DEM-20 m in comparison to DEM-1 m; (b) the impact of the friction coefficient (µ) was much greater than the friction coefficient ([Formula: see text]) on the results; (c) the effect of the terrain curvature activation on the results was not significant; (d) changing in inflow direction to up to ± 50 degrees did not cause a significant change in the overall results.

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Publication Details

Journal
Scientific Reports
Published
2025-10-17
DOI
https://doi.org/10.1038/s41598-025-20303-3
Primary Topic
Landslides and related hazards
Type
article
Field-Weighted Citation Impact
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article

Assessment of physical parameters impacts on debris flow modeling with RAMMS

Majid Galoie, Jihui Fan
Scientific Reports
Landslides and related hazards
article

Assessment of physical parameters impacts on debris flow modeling with RAMMS

Majid Galoie, Jihui Fan
article en

Abstract

The Rapid Mass Movement Simulation (RAMMS), requires input data such as DEM, the Voellmy-fluid friction coefficients, flow direction, and release information. To evaluate the uncertainties in RAMMS outputs using various input data, a real debris flow event was considered. After the calibration of the model, different scenarios were defined, which included different DEM cell sizes (1, 2, 3, 4, 5, 10, 15, and 20 m), different values of friction coefficients (the Dry-Coulomb type µ= [0.1, 0.2, 0.3]; the viscous-turbulent [Formula: see text]= [100, 200, 400, 800]), different directions of inflow (changes up to ± 50 degrees with a 10-degree interval), and active or inactive consideration of terrain curvature. The final results showed: (a) by increasing the DEM cell size, holding all other parameters constant, the accuracy of the model outputs (e.g. overall inundation area) reduced intensively which was up to 724% for DEM-20 m in comparison to DEM-1 m; (b) the impact of the friction coefficient (µ) was much greater than the friction coefficient ([Formula: see text]) on the results; (c) the effect of the terrain curvature activation on the results was not significant; (d) changing in inflow direction to up to ± 50 degrees did not cause a significant change in the overall results.

Scientific ReportsVol. 15(1)
Chinese Academy of Sciences (CN), Institute of Mountain Hazards and Environment (CN), Imam Khomeini International University (IR)
National Natural Science Foundation of China
Openalex Percentile: Top 60%
Landslides and related hazards
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