Measurements of outgoing radiation fluxes with spaceborne scanning nar
row and nonscanning wide field-of-vision radiometers are considered. T
he problem of data processing is discussed. Capacities of both methods
are compared. Outgoing radiation fluxes are measured within short-wav
e (SW) and long-wave (LW) ranges using spaceborne scanning and nonscan
ning sensors whose field-of-vision is oriented to the nadir. Both type
s of sensors yield a great deal of information (see e.g [1-3]). Effort
s to interprete the obtained data have been made since early 60s [2, 4
-10, 12]. Evolution of the equipment for satellite measurements of com
ponents of the Earth radiation balance (ERB) is in progress. In this c
onnection it is interesting to compare methods employed to measure out
going radiation by scanning and nonscanning spaceborne sensors.