Observations of Radio Emission of the Moon at 2.3 cm by the Pulkovo Large Radio Telescope
The measurement of the amplitude of variation of the brightness temperatureTaat the centre of the lunar disk enables, as is shown in [1], to evaluate the magnitude of the equivalent conductivity σ of the material of the lunar crust. The amplitude of variation of brightness temperatureTacan be determined with the aid of radio telescopes with high resolving power by direct measurements of the brightness temperatureTein the course of a lunation. Such measurements require that the area efficiency σ of the antenna and conditions of calibration of the receiving apparatus over the period of observations to be constant, and this is hard to ensure.Tacan also be determined by measuring the shift of the centre of gravity of radiationxu[2]†, resulting from the fact that the variable component of brightness temperature, in superimposing itself on the constant component, distorts the symmetry of the curves of equal light intensity (isophotes) relative to the central meridian, and shifts the point of maximum brightness away from the centre of the disk in the direction of the subsolar point, asTais a functionxu.