Wind induced errors in precipitation measurements result in systematic
deficits, which are particularly large when the precipitation falls a
s snow combined with high wind speed. The actual magnitude of the defi
cit can amount to more than half of the true precipitation. In order t
o correct for these deficits, newly developed statistical models for s
olid and mixed precipitation are presented; together with a correction
model for liquid precipitation presented earlier, a comprehensive sys
tem of correction models is now available. Statistical errors on the c
orrections are estimated.