Verplanck, Samuel VincentAdams, Eward Eagan2024-07-082024-07-082024-03Verplanck SV, Adams EE. Dynamic models for impact-initiated stress waves through snow columns. Journal of Glaciology. Published online 2024:1-15. doi:10.1017/jog.2024.260022-1430https://scholarworks.montana.edu/handle/1/18657The objective of this research is to model snow's response to dynamic, impact loading. Two constitutive relationships are considered: elastic and Maxwell-viscoelastic. These material models are applied to laboratory experiments consisting of 1000 individual impacts across 22 snow column configurations. The columns are 60 cm tall with a 30 cm by 30 cm cross-section. The snow ranges in density from 135 to 428 kg m−3 and is loaded with both short-duration (~1 ms) and long-duration (~10 ms) impacts. The Maxwell-viscoelastic model more accurately describes snow's response because it contains a mechanism for energy dissipation, which the elastic model does not. Furthermore, the ascertained model parameters show a clear dependence on impact duration; shorter duration impacts resulted in higher wave speeds and greater damping coefficients. The stress wave's magnitude is amplified when it hits a stiffer material because of the positive interference between incident and reflected waves. This phenomenon is observed in the laboratory and modeled with the governing equations.en-UScc-byhttps://creativecommons.org/licenses/by/4.0/avalanchessnow mechanicssnowArticle10.1017/jog.2024.26