Preliminary measurement of the stratospheric aerosol layer using multiwavelength laser radar (*=0.6943µm and 0.3471µm) are presented. This result suggested that there was noticeable change on the vertical distribution of size distribution and/or chemical composition of the aerosol particles. The contribution of Mie scattering component at *=0.3471µm to the total scattered light becomes apparently smaller than that at *=0.6943µm owing to the so-called "dependence of *-4 in Rayleigh scattering", and this enables us to search out easily the fitting point which is used to distinguish the Mie scattering component from the measured total scattering power intensity.