Forward scatter in the troposphere has been used for more than two decades as a means to communicate at meter and centimeter wavelengths over distances beyond the horizon. The increasing number of space and terrestrial links operating at increasingly higher frequencies has created a need to determine the probability of interference as a function of separation between services. With the improved resolution of narrow-beam antennas, bistatic systems can also be used to investigate meteorological parameters of the troposphere. By the use of synchronized antenna scanning at both ends of the path, it is poss'ible to study propagation mechanisms and to examine tropospheric structure and motion with an angular resolution previously not availablel,2. In the experiment described, measurements o f transmission loss at 15.7 GHz have been taken over a 500 km path and meteorological data obtained over a surface area 200 km long and 100 km wide at the center o f the path. Figure 1 illustrates the computer-controlled motion of the common volume of the antenna beams (center at P) during a great circle plane raster scan (xz plane) and a midpath plane raster scan (yz plane). Other types of scans are performed in addition to the xz plane and yz plane rasters to analyze particular characteristics of the troposphere, to measure cross-path wind speeds, and to simulate long-distance interference situations.A typical recording of a great circle plane raster is given in Figure 2. It consists o f 20 individual scans and lasts IO minutes. Several horizontally stratified layers are visible in the height range between 8 and 13 k m . Effectively no signals are received in those portions of the scans which are below the radio horizons (the dashed lines in Figure 2). Three-dimensional scanning of the bistatic system with high spatial and doppler resolution permits discrimination between turbulent scatter, hydrometeor scatter, and ducting. Also the effect o f antenna sidelobe coupling can be determined.Continuous recordings of cross-path wind speed, which are difficult to obtain with conventional meteorological instrumentation, have been obtained from upper levels of the troposphere over extended 2 0 0