Rain has long been categorized as a contaminant of altimeter data, but
little has been done previously to ascertain the magnitude and freque
ncy of its effect or its geographical distribution. Proceeding from re
cent analysis of ERS-1 data, and the insight gained, this paper addres
ses all these issues, highlighting the particular advantages of Topex'
s dual-frequency capability. The primary effect of rain is on the obse
rved backscatter values sigma(0) through attenuation of the radar sign
al. An empirical relationship is derived linking the observed sigma(0)
values at C band and K-u band. Through a series of case studies and g
lobal analyses, prominent departures from this relationship are shown
to be caused by regions of significant precipitation. As it is predomi
nantly the K-u-band returns that are affected, C band sigma(0,)s are l
ikely to be of great use for the determination of wind speeds in regio
ns or events of intense rain. The different attenuation rates give dua
l-frequency altimetry the potential to yield information on rain distr
ibution and intensity that complement that achievable by infrared sens
ors alone.