A study of the outgoing radiation from the atmosphere
A model of the atmosphere as homogeneous layers with the thickness of 100 m is considered. The influence of the altitude distribution of water vapor in the atmosphere on the power of the outgoing radiation in the 1300-1500 cm<sup>-1</sup> was determined The contribution of increasing the methane content in the layer and the height of this layer to the spectral regions 1238.690-1238.73, 1240.980-1241.020, and 1240.901-1240.949 cm<sup>-1</sup> of the outgoing radiation of the Earth is estimated.