The heat diffusion across magnetic islands is studied numerically and compared with analytical results. For a single island, the enhanced radial heat diffusivity, χ r , due to the parallel transport along the field lines is increased over a region of about the island width w. The maximum enhanced heat conductivity at the rational surface is proportional to w 2 (χ || χ ⊥ ) 1/2 for sufficiently high values of χ || /χ ⊥ , where χ || /χ ⊥ is the ratio between the parallel and the perpendicular heat diffusivity. For low ratios of χ || /χ ⊥ , however, the maximum value of χ r is proportional to w 4 χ || . In a locally stochastic magnetic field, χ r is again proportional to w 4 χ || for low χ || /χ ⊥ , which is in agreement with the analytical results. With increasing χ || /χ ⊥ , χ r is dominated first by the additive effect of individual islands and then by the field ergodicity.2