Evaluation of X-band polarimetric radar estimation of rainfall and rain drop size distribution parameters in West Africa

As part of the African Monsoon Multidisciplinary Analysis (AMMA) field campaign an X-band dual-polarization Doppler radar was deployed in Benin, West-Africa, in 2006 and 2007, together with a reinforced rain gauge network and several optical disdrometers. Based on this data set, a comparative study of several rainfall estimators that use X-band polarimetric radar data is presented. In tropical convective systems as encountered in Benin, microwave attenuation by rain is significant and quantitative precipitation estimation (QPE) at X-band is a challenge. Here, several algorithms based on the combined use of reflectivity, differential reflectivity and differential phase shift are evaluated against rain gauges and disdrometers. Four rainfall estimators were tested on twelve rainy events: the use of attenuation corrected reflectivity only (estimator R(Z(H))), the use of the specific phase shift only R(K-DP), the combination of specific phase shift and differential reflectivity R(K-DP,Z(DR)) and an estimator that uses three radar parameters R(Z(H), Z(DR),K-DP). The coefficients of the power law relationships between rain rate and radar variables were adjusted either based on disdrometer data and simulation, or on radar-gauges observations. The three polarimetric based algorithms with coefficients predetermined on observations outperform the R(Z(H)) estimator for rain rates above 10 mm/h which explain most of the rainfall in the studied region. For the highest rain rates (above 30 mm/h) R(K-DP) shows even better scores, and given its performances and its simplicity of implementation, is recommended. The radar based retrieval of two parameters of the rain drop size distribution, the normalized intercept parameter N-w and the volumetric median diameter D-m was evaluated on four rainy days thanks to disdrometers. The frequency distributions of the two parameters retrieved by the radar are very close to those observed with the disdrometer. N-w retrieval based on a combination of Z(H)-K-DP-Z(DR) works well whatever the a priori assumption made on the drop shapes. D-m retrieval based on Z(DR) alone performs well, but if satisfactory Z(DR) measurements are not available, the combination Z(H)-K-DP provides satisfactory results for both D-m and N-w if an appropriate a priori assumption on drop shape is made