The Wilson wind‐generated source level densities and the ASTRAL propagation loss model are combined to form a wind‐generated noise model. The model treats storms as a geographically distributed source and is capable of modeling both distant and local storm noise. Model estimates are compared with omnidirectional measurements from the northeastern Pacific Ocean at five frequencies and three receiver depths. The results are very good and indicate the necessity of modeling both shipping and wind‐generated noise in comparisons with measured data.