Jouvet, GuillaumeHuss, MatthiasBlatter, HeinzPicasso, MarcoRappaz, Jacques2010-11-302010-11-302010-11-30200910.1016/j.jcp.2009.05.033https://infoscience.epfl.ch/handle/20.500.14299/59945WOS:000268898200020Due to climatic change, many Alpine glaciers have significantly retreated during the last century. In this study we perform the numerical simulation of the temporal and spatial change of Rhonegletscher, Swiss Alps, from 1874 to 2007, and from 2007 to 2100.Ice flowFinite elementsVolume of fluidFree surfaceFree-SurfaceFlowline ModelGlacierSwitzerlandFlowsIceCavitationEvolutionDynamicsClimateNumerical simulation of Rhonegletscher from 1874 to 2100text::journal::journal article::research article