Selection of microwave bands for global snow detection

Microwave radiometers and scatterometers as all-weather and day-and-night sensors are excellent tools for the reliable, regular observation of dynamic features of the surface of the earth. The various hydrologic states, the development of the metamorphism, the water equivalent and other parameters of the snow cover cause a very distinct spectral behaviour of the microwave emission and backscattering.The results of a long-term ground-based investigation of the microwave radiation properties along with classical determinations of the snow parameters during five seasons on an alpine test area allow the definition of an optimum package of microwave passive and active sensors for the global monitoring of the snow cover.Additionally it has been demonstrated that the utilization of the Nimbus-7 Scanning Multi-channel Microwave Radiometer data permit the production of large scale maps of the extent of dry snow, the estimated water equivalent of dry snow and the areas changing between frozen and wet snow.