The results of numerical modeling of local atmospheric circulation over a forest fire zone are considered. Two numerical models of the atmospheric boundary layer are used as the basic ones. One model has a detailed resolution along the horizontal, and there is a possibility of explicitly reproducing the ensemble of large convective vortices. The other model is hydrostatic and it is used for studying large-scale transfer of a smoke jet. The results of numerical experiments for a typical fire in middle latitudes are presented.