The distributions of dust temperatures and mean radiation intensities
in axially symmetric dusty disks are calculated within the framework o
f the flux-limited diffusion approximation. A multi-component dust mod
el, consisting of amorphous carbon and silicate grains, which are coat
ed with ''dirty ice'', is employed. After determination of the dust te
mperatures a ray-tracing procedure is used to calculate the spectral a
ppearance of the disk at varying inclinations and to produce isophote
maps at selected frequencies. The spatial distribution of dust tempera
tures resulting from these calculations reflect the shape of a disk's
density distribution and do not display a simple (distance)(-a) power
law. The spectra calculated from the same disk model at different incl
inations can vary over a wide range. It is therefore often not possibl
e to derive parameters of a disk - in particular its evolutionary stat
e - from the spectrum alone. It is not recommended to infer the existe
nce of planets by using simple temperature power law fits to disk spec
tra in combination with simple power law dust opacities.