Handout (2.0 MB)
In the present work, an algorithm to retrieve microphysical parameters of rainfall using the MIRA-35C is developed. Doppler spectra are used to calculate the drop size distribution (DSD), and the different microphysical parameters, such as rainfall intensity and liquid water content. Also, algorithms for correction of wet antenna attenuation and path-integrated attenuation are included. These algorithms are necessary for the correct estimation of precipitation.
Preliminary results, for four rainfall events, indicate that the attenuation caused by wet antenna can reach 9 dB generating errors of around 400%. With attenuation correction, the rainfall intensity near the surface is compared with in situ data (rain gauge and disdrometer). The analysis of the precipitation estimated by the radar versus rain gauge, for the cases of study, show in average an error of 2 mm and an absolute relative error of 29%. The wet antenna attenuation correction algorithm is still in development; it is expected that the results can be greatly improved with further studies.
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