“…The tensile strength of the ice is in this article assumed to be around 3.0 MPa, which is a maximum value commonly used in the literature for freezer ice (Meng and Guo, n.d.;Petrovic, n.d.;Druez et al, 1986;Reich et al, 1994;Andrews and Lockington, 1983). After initiation, in most cases, the fracture instantaneously propagates to the interface thanks to the unstable behavior of the crack (second step of the fracture mechanism) (Palanque et al, 2021). This is explained using the Griffith theory on fracture propagation in brittle materials (Lawn, 1993;Anderson, 2005), which is detailed in the next part of the paper.…”