Long-term precipitation and snow-cover measurements were carried out to est
imate the areal pattern of precipitation in a small, rugged Swiss pre-Alpin
e basin. The dense networks used consisted of 34 storage gauges and 32 pit
gauges with orifice parallel with slope, the latter being corrected for wet
ting losses. Consequently, the corrected data was very near to the "true" p
recipitation at a particular point. In the winter season also snow-cover ch
aracteristics were measured at 11 locations. Altitude turned out to be the
best overall predictor for corrected data (R-2 = 0.67) and longitude for un
corrected data (R-2 = 0.67 vs only 0.58 for altitude!). The combination of
altitude, longitude and latitude explains almost 75% of the spatial varianc
e of summer season precipitation and snow-cover characteristics. However, t
he three variables used in the analysis were found to be interrelated, part
icularly in networks of storage gauges and snow-cover measurements (R-2 = 0
.40-0.70).