Calibration issues of dual-polarization radar measurements

Techniques for the absolute calibration of radar reflectivity Z and differential reflectivity Z(DR) measured with dual-polarization weather radars are examined herein. Calibration of Z is based on the idea of self-consistency among Z, Z(DR), and the specific differential phase K-DP in rain. Extensive spatial and temporal averaging is used to derive the average values of Z(DR) and K-DP for each 1 dB step in Z. Such averaging substantially reduces the standard error of the K-DP estimate so the technique can be used for a wide range of rain intensities, including light rain. In this paper, the performance of different consistency relations is analyzed and a new self-consistency methodology is suggested. The proposed scheme substantially reduces the impact of variability in the drop size distribution and raindrop shape on the quality of the Z calibration. The Pew calibration technique was tested on a large polarimetric dataset obtained during the Joint Polarization Experiment in Oklahoma and yielded an accuracy of Z calibration within 1 dB. Absolute calibration of ZDR is performed using solar measurements at orthogonal polarizations and polarimetric properties of natural targets like light rain and dry aggregated snow that are probed at high elevation angles. Because vertical sounding is prohibited for operational Weather Surveillance Radar-1988 Doppler (WSR-88D) radars because of mechanical constraints, the existing methodology for ZDR calibration is mod ified for nonzenith elevation angles. It is shown that the required 0.1-0.2-dB accuracy of the ZDR calibration is potentially achievable.