Scan channels on the NIMBUS 7 Earth Radiation Budget (ERB) instrument sample radiances from underlying earth scenes at a number of incident and scattering angles. A sampling excess toward measurements at large satellite zenith angles is noted. Also, at large satellite zenith angles, the present scheme for scene selection is causing many observations to be classified as cloud, resulting in higher flux averages. Thus, the combined effect of sampling bias and scene identification errors is to overestimate the computed albedo. It is shown, using a process of successive thresholding, that observations with satellite zenith angles greater than 50¿--60¿ lead to incorrect cloud identification. Elimination of these observations has reduced the albedo from 32.2 to 28.8%. This reduction is very nearly the same and in the right direction as the discrepancy between the albedoes derived from the scanner and the wide field-of-view (WFOV) channels.