Spectral flux density calibration of a meridian instrument is carried out using a grid of calibration objects that relatively uniformly cover the available sky region in the elevation angle. By observing objects at different elevations, the calibration curve of the conversion factor between antenna temperature and spectral flux density versus the antenna elevation angle is constructed. This curve reflects variation of antenna effective area and short-wave atmospheric absorption depending on radio source elevation allowing for actual aberrations due to the transverse offset of the primary feeds from the electric axis of the telescope. To calculate spectral flux density, a technique described in detail in Aliakberov et al., 1985 and Udovitskiy et al., 2016 is used.