Recent studies using classical precipitation models to follow experimental precipitation kinetics in Al-Sc alloys have concluded that an explicitly time-and temperature-dependant interfacial energy must be adopted to explain the observed precipitation kinetics. An alternative explanation for the precipitation kinetics based on vacancy-enhanced diffusivity is proposed in this work. This method, combined with a classical Kampmann-Wagner (KWN) class model, has allowed us to reconcile the kinetics of nucleation, growth, and coarsening in an Al-Mg-Sc alloy using a single value for the interfacial energy in the temperature range 250°C to 350°C.