Retrieval methods to estimate the effective radius (r(e)) and the liquid water content (LWC) of stratocumulus clouds from radar and lidar observations are presented here. The retrieval of r(e) is accomplished by combining radar and lidar observations by means of a Z/alpha - r(e) relation, which is derived from the measurements of in-situ particle probe instruments. The retrieval of LWC, on the other hand, is done solely on the basis of radar observations. However, when plotting a Z-LWC diagram, there was too much scatter, preventing a direct derivation of a Z-LWC relation. It appears that the deviating points in the Z-LWC scatter diagram are mainly caused by the size distributions that have a rather large r(e). By filtering out these distributions, the scatter in the Z-LWC diagram is significantly reduced and an empirical Z-LWC relation is derived. The estimates of r(e) and LWC using airborne radar and lidar show reasonably good agreements with the profiles measured insitu. A comparison of the LWC estimated from ground-based radar data, integrated over the cloud height, with the liquid water path provided by a radiometer also shows good agreement, with a general offset of about 50 g m(-2) (C) 2000 Elsevier Science Ltd. All rights reserved.
