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Radar-lidar synergy for the retrieval of water cloud parameters. Herman Russchenberg, Oleg Krasnov. International Research Centre for Telecommunication and Radar. radar. radiometry. lidar. Ground based observations. Are power laws useful?. Dropsize distribution.
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Radar-lidar synergy for the retrieval of water cloud parameters Herman Russchenberg, Oleg Krasnov International Research Centre for Telecommunication and Radar
radar radiometry lidar Ground based observations
Are power laws useful? Dropsize distribution Very sensitive to tail of dsd
Common opinion: No, there is too much scatter due to drizzle unless we can identify the drizzle droplets somehow...
drizzle “transition” drizzle A million droplets of 10 micron give the same radar reflection as one droplet of 100 micron! A million droplets of 10 micron contain a thousand times as much water as one one droplet of 100 micron... And so: one drizzle droplet changes the reflectivity significantly without changing the liquid water content non-drizzling
Radar reflection Drizzling Non-drizzling Coarse classification
Radar and lidar observables in relation to microphysics of water clouds Radar-lidar ratio vs effective radius Radar reflectivity vs liquid water content
65.0 % 27.1 % 7.9 % Statistics of cloud types, Cabauw
61.4 % 29.3 % 9.3 % Statistics of cloud types, Chilbolton
63.5 % 27.8 % 8.7 % Statistics of cloud types, Palaiseau
-20 dBZ -35 dBZ 63.5 % 8.7 % 27.8 % Statistics of cloud types, all sites
Climatology or calibration? Site-specific thresholds Averaged CloudNet thresholds
The difference between the radar/lidar LWP retrievals and microwave radiometer After filtration out values of both LWP > 400 g/m^2
The difference between the Radar/lidar retrievals and ECMWF NWPM LWP After filtration out values of both LWP > 400 g/m^2
Outlook • Refine statistics • Refine thresholds • Application to ARM data • Apply to CloudSat – Calipso • Combine with IPT