A new evolutionary drag coefficient for landslides is derived as a function of a dimensionless acceleration number, representing energy inefficiency and automatically adjusting with flow dynamics.
(2026): A comprehensive approach to predicting low-angle glacier detachment-induced river damming: Insights from the Zelunglung Glacier
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The landslide drag
A new evolutionary drag coefficient for landslides is derived as a function of a dimensionless acceleration number, representing energy inefficiency and automatically adjusting with flow dynamics.