“…Besides the classical finite element method (FEM) and the finite difference method (FDM), diverse new numerical approaches have been proposed (Soga et al, 2016). Smooth particle hydrodynamics (Cascini et al, 2014) has been used to simulate channelized landslides of flow type; the material point method (Soga et al, 2016;Abe et al, 2013;Marcelo et al, 2016;Bandara et al, 2016) can describe the whole process of landslide movement using hydromechanical coupling; the discrete element method has been used to model the instability of jointed rock slopes (Dong et al, 2015;Huang et al, 2015); and the finite element method with Lagrangian integration points (FEMLIP; Cuomo et al, 2013) has been developed from the particle-in-cell method (Harlow, 1964;Moresi et al, 2002Moresi et al, , 2003 and satisfies the two requirements for simulating the complete evolution of landslides: precise tracking of internal variables and the ability to solve large displacements (Li et al, 2016(Li et al, , 2018a. In contrast to the material point method, the numerical weight of material particles used in the FEMLIP method is updated at each time step, leading to an acceptable calculation cost, owing to the use of an implicit solver (Li et al, 2018a).…”