While radar polarimetry has shown improvements in data quality, the accuracy in estimating rainfall rate remains limited by the calibration especially for reflectivity at horizontal polarization (ZH) of the radar. Calibration of ZH can be achieved using the relationship between ZH, differential reflectivity (ZDR), and specific differential propagation phase (KDP). However, ZDR and ZH measurements can be decreased by rain attenuation along the radial direction especially for radars operating at C-band or higher frequencies. Thus, in this study, an attenuation correction is made for the two measurements before the calculation of theoretical KDP, which is then integrated in the radial direction to yield a theoretical differential propagation phase ( ΦDP). Differences between theoretical and observed ΦDP at the end of rain path are attributable to the bias in ZH measurements. Once the system bias in ZH measurements is determined, this method can also estimate attenuation due to both the wet radome and heavy rainfall simultaneously in ZDR and ZH measurements.