Radar observations of precipitation profiles from space are simulated in or
der to evaluate the impact of precipitation incoherent backscattering upon
radar returns above 10 GHz at nadir. Spaceborne and airborne radar frequenc
ies at 13.8, 24, and 35 GHz are chosen for carrying out simulations at nadi
r. Realistic precipitation profiles are extracted from a microphysical meso
scale cloud model simulation and averaged with respect to classes of surfac
e rainrate. The classical radar equation is reformulated taking into accoun
t the multiple scattering phenomenon through a general definition of the ap
parent reflectivity. Numerical results show that opposite effects are due t
o the combination of path attenuation and multiple scattering. When first-o
rder scattering approximation holds, path attenuation is the predominant co
ntribution and tends to reduce the equivalent reflectivity, while multiple
scattering tends to increase it, especially in the cloud regions characteri
zed by large albedo. For intense rainfall cases the rainrate profiles can b
e significantly overestimated when derived from apparent radar reflectivity
simply corrected by two-way single-scattering path attenuation. (C) 2000 E
lsevier Science Ltd. All rights reserved.