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Work Package 2 – Overview of instrumentation, data gathering and calibration issues Lidar Calibration Ewan O’Connor, Anthony Illingworth and Robin Hogan Progress meeting 3 –Reading – 24-25 Oct 2002
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Calibration technique ’=1/2 k Use Mie theory for spherical droplets. k is constant for cloud droplets (D=8-30 m).
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Multiple scattering Calculate as a function of range using Eloranta’s model (1998). Need to know laser divergence and telescope FOV.
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Aerosol k in aerosol variable therefore extinction unknown effect on calibration unknown Current solution: Reject profile for calibration if a > than some predetermined value
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Validation – UV Raman lidar Calibrate UV Raman lidar with molecular backscatter. To validate – need to calculate atmospheric transmission at both wavelengths and the value of for each instrument.
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Validation – UV Raman lidar Calibrate UV Raman lidarCompare calibrated CT75K ceilometer
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Validation – UV Raman lidar Step 1. Calibrate both lidars Step 2. Adjust for differences in atmospheric transmission Step 3. Adjust for differences in multiple scattering
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Validation in space – LITE
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CT75K – solar background
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