Longwave radiation in snow-covered alpine environments was investigate
d based on LOWTRAN7 calculations, The irradiance from the sky and from
the surrounding topography were determined separately in order to det
ect the influence of the topography on longwave radiation balance. Sen
sitivity studies showed that the irradiance from the surrounding terra
in is determined primarily by the atmospheric conditions within the in
vestigated area and by the surface temperature of the surrounding terr
ain. In snow-covered environments, the air temperature is usually abov
e the snow surface temperature and the effects of the air between the
topography and the receiving surface may be relevant. Longwave irradia
nce from the surrounding terrain is an important component of the ener
gy balance at the snow surface on inclined slopes and should be consid
ered for areal investigations. A simple parameterization that accounts
for the effects of the air is proposed for efficient calculation of l
ongwave irradiance from snow-covered topography.