This paper addresses the problem of finding a parametric form for the
raindrop size distribution (DSD) that 1) is an appropriate model for t
ropical rainfall, and 2) involves statistically independent parameters
. Such a parameterization is derived in this paper. One of the resulti
ng three ''canonical'' parameters turns out to vary relatively little,
thus making the parameterization particularly useful for remote sensi
ng applications. In fact, a new set of Gamma drop-size-distribution-ba
sed Z-R and k-R relations is obtained. Only slightly more complex than
power laws, they are very good approximations to the exact radar rela
tions one would obtain using Mie scattering. The coefficients of the n
ew relations are directly related to the shape parameters of the parti
cular DSD that one starts with. Perhaps most important, since the coef
ficients are independent of the rain rate itself, the relations are id
eally suited for rain retrieval algorithms.