Errors arise when using conventional radar reflectivity, Z, to estimate rai
nfall rate, R,and these can be particularly severe during severe convective
storms; the very events when accurate estimates are needed so that action
can be taken to mitigate the effects of flooding. Concentration is on three
problems associated with heavy rainfall: hail, attenuation and absolute ca
libration of the radar, and consider how polarisation radar parameters, dif
ferential reflectivity, Z(DR), and specific differential phase shift K-DP,
might lead to their alleviation. It is essential to consider the fundamenta
l limits to the accuracy with which these parameters can be estimated. If Z
DR can be measured to an accuracy of 0.2 dB, then it provides a measure of
mean raindrop shape which is sufficiently precise to improve rainrate estim
ates. This can be achieved at S-band (10 cm), but seems very difficult for
operational C-band (5 cm) radars; differential attenuation by the heavy rai
n introduces a negative bias into Z(DR) which increases with range. However
, the magnitude of this bias at C-band can then be used to correct for the
total attenuation of Z. Differential phase, K-DP, has the advantage that it
is a phase measurement and so is unaffected by attenuation. It only respon
ds to the rainfall and is unaffected by the hail, but K-DP is a noisy param
eter and is only useful for heavy rainfall above 30-60 mm hr(-1). Fortuitou
sly, K-DP and Z(DR) are not independent and one use of K-DP and Z(DR) may w
ell be to exploit this redundancy to identify rain areas as opposed to hail
, and in rainfall to use the redundancy to provide an automatic calibration
of the absolute reflectivity, Z, to 0.5 dB (12%). Finally, the noisy chara
cter of both ZDR and KDP together with the low level of the co-polar correl
ation coefficient provide the first reliable means of detecting and removin
g anomalous propagation which is a major operational problem for all weathe
r radars.