The forward model relies on the hydrometeor scattering properties generated using the discrete dipole approximation technique. The model can compute reflectivity and attenuated reflectivity across diverse radar instruments and zenith angles as long as the instrument-specific coefficients for CRTM are available. Rigorous evaluation utilizing CloudSat measurements reveals substantial agreement between simulations and observations, contingent upon consistency between hydrometeor input profiles and measured reflectivity profiles.
Current efforts include the integration of the forward radar simulator into the Joint Effort for Data assimilation Integration (JEDI) framework. This integration not only includes generating new observation formats for spaceborne radars, but also adapting the Unified Forward Operator to effectively process radar measurements. This ongoing initiative provides new capabilities for the assimilation of spaceborne radar measurement, which can lead to improving the representation of precipitation and clouds in the NWP models.
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