Descriptive statistics of fade slope from the INTELSAT VI beacon data at 11
.198GHz and 42.8 degrees elevation are presented. Results indicate a direct
positive correlation between the mean values of fade slope and attenuation
and show that individual rain events have higher fade slope with deeper fa
de depths. The absolute fade slopes can be best approximated by a log-norma
l distribution. Positive and negative fade slopes are symmetrically distrib
uted and the distribution becomes flatter at higher attenuation levels.