The present report discusses a structure dependent model of emissivity of s
now cover. A snow cover was represented by a medium comprised of discrete s
catterers. In the case of dry snow, ice grains stood for scatterers. For we
t snow, two geometrical configurations of the water component were consider
ed: I is a mixture of ice grains and water drops; II is a mixture of ice gr
ains covered with water film and water drops. Scatters were assumed to have
a spherical from and the lognormal distribution of sizes. Calculations of
radiobrightness temperature of snow cover were made using data of glaciolog
ical measurements of its physical parameters and microstructure. Results of
calculations were compared with measurements of radiobrightness temperatur
e at various states of the snow cover.