To link multi-frequency radar observations to snow microphysics retrievals of physical properties of snowflakes, namely mass-dimensional relations, terminal velocity- diameter and shapes and fall velocity were carried out. To insure that the retrievals are meaningful different methods utilizing different sets of instruments were applied for the retrievals. For example, mass-dimensional relations were retrieved using two different instruments, NASA Particle Image Package and 2D-video disdrometer, by utilizing Böhms method. At the same time these retrievals are validated by comparing measured X-band radar reflectivity and precipitation liquid equivalent accumulation to ones calculated from observed particle size distributions and retrieved mD. A number of other cross checks was applied to insure consistence of different retrievals. After this step, different aspects of multi-frequency radar retrievals of snow microphysics were tested. For example, a connection between dual-frequency ratios and median volume diameter in a variety of snow cases was checked. It was found that performance of X/Ka and Ka/W retrievals differ and the biggest difference is observed for low-density aggregates. Other findings of this study will also be presented at the conference.