Abstract
Over the past several years a cloud lidar system (CLS) has been deployed on high altitude aircraft cloud observation missions. The instrumentation configuration and some initial data acquired in Fall 1979 have been previously reported.1,2 In May-June 1981 a further set flights were undertaken in conjunction with the large scale CCOPE experiment. A modified configuration, shown in Fig. 1, was employed for these later flights. The major additions to the instrument were a 1064 nm detector to supplement the dual polarization 532 nm detectors and also an increase to a 20 MHz data acquisition bandwidth.
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