We suppose the transport of energy in a sunspot (or pore) is described
by a diffusion process. The thermal conductivities in the spot and it
s surroundings are assumed to be constant and isotropic, but with a re
duced conductivity in the spot. The sunspot and the ambient medium are
. represented by semi-infinite strips of variable depth, with one comm
on boundary. This interface is a plane inclined at an arbitrary angle
with respect to the vertical in order to simulate the inclined magneti
c field at the umbral/penumbral, penumbral/photospheric or pore/photos
pheric boundary. We show that the region with high conductivity below
the interface produces a thermal disturbance in the surface layers of
the umbra which manifests itself as a temperature enhancement at the u
mbral surface in a region near the boundary, resulting in a decreased
temperature contrast across the surface. The thermal disturbance in th
e neighboring medium is confined to a very small region.