Analysis of data from the C-band UK operational network polarization radars using hybrid mode shows excellent performance in light to moderate rain, with value of the co-polar correlation (ρHV) exceeding 0.99, the linear depolarization ratio (LDR) below -30dB, ZDR is estimated to better than 0.2dB, and φdp to within a couple of degrees; in the bright band ρHV falls to 0.9 as expected from the mixture of wet oblate melting snowflakes and raindrops. The performance in heavier attenuating rainfall is a cause for some concern. In theory in heavy rain φdp should increase with range as a result of attenuation and be accompanied by increasingly negative values of ZDR due to the differential attenuation; any values of ρHV below 0.9 where Z is very high should indicate Mie scattering hail, and in any lighter rain behind the storm ρHV should recover to 0.99. The observed behavior is rather different. We find that whenever Z exceeds 50dBZ along a ray and φdp is above 45deg then ρHV always falls to 0.9 or lower, and stays at this low level in the lighter rain behind the storm; in this light rain with low ρHV, the values of ZDR are far more negative than theoretically predicted from φdp. We suspect that for a C-band radar operating in hybrid mode, once φdp exceeds 45deg, the effects of cross-talk between the H and V returns may render the polarization parameters unreliable and they should be treated with caution.