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Lidar network observations of Cirrus morphological and scattering properties during the International Cirrus Experiment 1989: The 18 October 1989 case study and statistical analysis

By U. Wandinger, C. (GKSS-Forschungszentrum Geesthacht GmbH (Germany). Inst. fuer Physik) Weitkamp, J. Boesenberg, M. Riebesell, W. Michaelis, A. Ansmann, Hamburg (Germany). Meteorologisches Observatorium) K. (Deutscher Wetterdienst Klapheck, 91 - Palaiseau (France). Lab. de Meteorologie Dynamique) L. (Ecole Polytechnique Menenger, P.H. Flamant, S. Elouragini, 59 - Villeneuve-d'Ascq (France). Lab. d'Optique Atmospherique) G. (Lille-1 Univ. Brogniez, Hamburg (Germany)) P.Y. (Max-Planck-Institut fuer Meteorologie Thro, C. Senff, H. Linn and GKSS-Forschungszentrum Geesthacht GmbH (Germany)


Four lidars, located roughly 75 km from each other in the inner German Bight of the North Sea, were used to measure geometrical and optical properties of cirrus clouds during the International Cirrus Experiment 1989 (ICE '89). A complete cirrus life cycle was observed simultaneously with three lidars during a case study on 18 October 1989. Time series of particle backscatter, depolarization-ratio height profiles, cloud depth, optical thickness, and of the cirrus extinction-to-backscatter, or lidar, ratio describe the evolution of the cloud system. A two-wavelength lidar measurement was performed and indicates wavelength independence of ice-crystal scattering. The optical and geometrical depths of the cirrus were well correlated and varied between 0.01 and 0.5 and 100 m and 4.5 km, respectively. Although the evolution of the cloud deck was similar over the different observation sites, cirrus geometrical, scattering, and microphysical properties were found to vary considerably within the lidar network. A statistical analysis of ice-cloud properties is performed based on 38 different cirrus cases sampled during ICE '89. Cirrus formation was found to start at the tropopause in most cases. Ice clouds, measured at high midlatitudes (around 54 N), were thin with mean optical and geometrical depths mainly below 0.4 and 2 km, respectively. A good correlation between mean cloud optical and geometrical thickness, and a weak decrease of the mean optical depths with temperature was observed. (orig.)Also published in: Journal of Applied Meteorology (1993) v. 32, p. 1608-1622Available from TIB Hannover: RA 3251(93/E/74) / FIZ - Fachinformationszzentrum Karlsruhe / TIB - Technische InformationsbibliothekSIGLEDEGerman

Year: 1993
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Provided by: OpenGrey Repository
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