Rain gauges and x-band radar hourly comparison under complex orographic conditions in Reunion Island

International audience ; Located in the South-West Indian Ocean, Reunion Island is a volcanic island known for its complex terrain. The island's topography is characterized by steep mountains and deep valleys, which can create significant spatial variability in precipitation patterns. As a result, rainfall measurements can vary considerably across different areas of the island. As part of the ESPOIRS project, a transportable X-band Doppler radar with dual polarization was acquired to study the influence of orography on precipitation in Islands of the Southwest Indian Ocean. During the first campaign of this project, the radar was installed in the Southern coastal region of La Reunion. Hence, the first aim of this present study is to evaluate the accuracy and reliability of this radar for quantitative precipitation estimation. This will be achieved by comparing the radar data with rain gauges data collected during extreme precipitation events that occurred in La Reunion in 2022. This study also highlighted the challenges of using a X-band radar in complex orographic conditions. For instance the blockage of the radar beam inducing a significant altitude difference between the radar sampled area and the rain gauges located in valleys.Likewise, the attenuation of the X-band radar signal due to heavy precipitations close to the radar is an important parameter to account in order to effectively exploit the measurements far from the radar. To correct for the attenuation of the radar reflectivity, we used two different approaches: i) the Hitschfeld and Bordan algorithm (1954), which is mainly used for single-polarization radar, and ii) the Philinear algorithm, which relies on the linear relationship between reflectivity and differential phase PHIDP. The results indicate that in heavy rainfall, the Philinear algorithm is more effective than the Hitschfeld and Bordan algorithm. Then, to convert radar observations into rain rates (R), two empirical models were used: a) rain rate-reflectivity relationship R(ZH), and b) rain ...