Statistical downscaling of precipitation from the large scales of meteorolo
gical models to the characteristic response scales of small catchment basin
s needs to correctly preserve the anomalous scaling laws observed in real r
ainfall. Multifractal behaviour of precipitation in space is investigated o
n a set of rainfall fields obtained by a high resolution simulation with a
limited area model for numerical weather prediction and on two sets of rada
r measures of rainfall during the GATE campaign. Some sets of synthetic rai
nfall fields were generated applying a multifractal model based on a wavele
t expansion with coefficients extracted by a log-Poisson random cascade, an
d results of comparisons with the GATE rainfall fields are presented. (C) 1
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