We investigate in this paper the variation in power of VHF radar vertical e
choes as a function of atmospheric humidity. We find that the echoes are gr
eatest in air of moderate (30-70%) humidity, and least in very dry or near-
saturated air. Compared to moderate humidities, the standard model for rada
r echoes, based on potential refractivity, overpredicts the echo power at h
igh relative humidity by similar to 10 dB. We propose that this is due to t
he effect of precipitation in suppressing small-scale humidity gradients. A
model which assumes complete suppression underpredicts the observed power
drastically, showing that precipitation can only remove a part of the small
-scale structure in refractivity which is caused by fluctuations in humidit
y.