Table 1. Parameters used in the dv/v modeling.
Parameter | Symbol | Value | Reference |
Glaciostatic pressure | Pg | 1600 Pa | From data |
Ice area | Si | 6.5 × 1011 m2 | From data |
Gravitational acceleration | g | 9.81 m/s2 | |
Pressure field wave number | k | 2π/(60 km) | Jiang et al. (11) |
Depth of investigation | z | 5 km | From data |
S-wave velocity | Vs | 3300 m/s | Kumar et al. (56) |
Vp/Vs ratio | Vp/Vs | 1.8 | Kumar et al. (56) |
Upper-crust density | ρc | 2700 kg/m3 | Schmidt-Aursch and Jokat (57) |
P-wave velocity | Vp = Vs(Vp/Vs) | 5940 m/s | |
Poisson’s ratio | ν | 0.2768 | |
Young’s modulus | E | 7.5 × 1010 Pa | |
Mantle viscosity | η | 1021 Pa⋅s | |
Viscoelastic relaxation time | T | 1011 s | |
Lamé’s first parameter | λ | 3.65 × 1010 Pa | |
Shear modulus | μ | 2.94 × 1010 Pa | |
Murnaghan constant | m | −2.77 × 1016 Pa | From inversion |
Distance from the ice | x | 12.5 km | |
Biot’s coefficient | α | 0.7 | Tsai (34) |
Hydraulic diffusivity of the crust | Kc | 0.5 m2/s | Shapiro et al. (58) |
Angular frequency | ω | 2π/(365 days) | |
Till layer thickness | zt | 2.85 m | From inversion |
Hydraulic diffusivity of till | Kt | 5 × 10− 6 m2/s | Iverson et al. (38) |