Handout (1.6 MB)
Furthermore, during most of the GPM/GV field campaigns the microwave radiometer ADMIRARI has been taking measurements along specific RHI scans at different radar frequency bands, e.g. X-band at CHUVA, C-band at LPVEx, MC3E and GCPEx. A dual-wavelength approach has also been pursued in cases like GCPEx and at the CHILL radar facility (CHILL and D3R radars) and recently at Jülich research center in Germany (X- and Ka-band radars). These observations allow to reconstruct a set of radar polarimetric variables along the ADMIRARI line of sight, and built-up a multi-sensor multi-frequency database. The reconstruction of the rain field within the ADMIRARI beam will leave the cloud liquid water field as a last unknown. Most of the cloud liquid content is located above the cloud base, which can be detected by either a ceilometer or be retrieved independently by the radiometer, leading to a further reduction of the degree of freedom of the problem. By means of 3D polarimetric radiative transfer simulations a set of synthetic observations will be produced to be used as a first guess in the frame of a optimal estimation theory (OST) retrieval approach.
The feasibility to built the OST capable to reconstruct precipitating parameter will be presented. The retrieval will use data from the polarimetric C/X-band radars, and will produce estimations for DSD and rain water content including error assessments. Such a closure study is a direct counterpart of the attempt of coherently integrating active and passive microwave instruments as a support study for developing multi-sensor algorithms for ground validation.
Supplementary URL: www2.meteo.uni-bonn.de/admirari