In this study we illustrate the improved retrievals of rain and snow facilitated by Doppler radar using case studies from aircraft and ground-based Doppler radar observations. Airborne measurements from the TC4 field campaign are used to show improved estimates of drop size and number concentration in tropical stratiform rain, demonstrating clear differentiation between the microphysics of warm rain and rain from melting ice. Ground-based observations from an ARM mobile facility deployment are used to demonstrate the use of Doppler velocity to estimate the density and morphology of snow particles from their terminal velocities, with insights into aggregation and riming processes in mixed-phase cloud. Finally, we demonstrate synergy retrievals from A-Train data, and consider where the improvements in snow and rain estimates from EarthCARE’s Doppler radar are likely to have the most impact on global retrievals of cloud and precipitation.
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