“…Since P wave propagation speeds depend on density and elastic moduli, the elastic modulus of snow can be derived from acoustic wave propagation experiments (AC) from first principles and are considered as most consistent (Mellor, ) due to high frequencies and small amplitudes. Such experiments invariably result in significantly higher values, on the order of 100 MPa (Capelli et al ; Smith, ). Alternatively, the elastic properties can also be derived from finite element calculations using the reconstructed 3‐D microstructure from micro‐computed tomography (CT) (e.g., Köhle & Schneebeli, ; Schneebeli, ; Srivastava et al, ; Wautier et al, ).…”