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A SPONTANEOUS RAYLEIGH-BRILLOUIN SCATTERING EXPERIMENT FOR THE CHARACTERIZATION OF ATMOSPHERIC LIDAR BACKSCATTER (TN4 part 3)
The difference between the theoretical Rayleigh-Brillouin lineshape and the measured lineshape fr...
J de Kloe, A Stoffelen | Year: 2009
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ADM-Aeolus Quasi Real-Time and Near Real-Time Wind Profiles
ESA’s Atmospheric Dynamics Mission (ADM), called Aeolus, is to launch the first spaceborne Dopple...
A Stoffelen | Year: 2009
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Precipitation type from the Thies disdrometer
A relatively new instrument on the market of Present Weather Sensors is the disdrometer from Thie...
HI Bloemink, E Lanzinger | Conference: WMO Technical Conference on Instruments and Methods of Observation | Organisation: WMO | Place: Bucharest, Romania | Year: 2005 | First page: 0 | Last page: 0
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SCIAMACHY monitoring factors: observation and end-to-end correction of instrument performance degradation
SCIAMACHY (SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY) is a grating sp...
K Bramstedt, S Noël, H Bovensmann, JP Burrows, C Lerot, LG Tilstra, G Lichtenberg, A Dehn, T Fehr | Conference: Atmospheric Science Conference | Organisation: ESA-ESTEC | Place: Barcelona, Spain | Year: 2009 | First page: 0 | Last page: 0
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The effect of reported high-velocity small raindrops on inferred drop size distributions and derived power laws
It has recently been shown that at high rainfall intensities, small raindrops may fall with much ...
H Leijnse, R Uijlenhoet | Status: published | Journal: Atm. Chem. Phys. | Volume: 10 | Year: 2010 | First page: 6807 | Last page: 6818 | doi: 10.5194/acp-10-6807-2010
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