ИСТИНА

Greenhouse gases and aerosols are the most important components of the cloudless atmosphere that affect the variability of atmospheric radiation, and an increase in their concentration due to anthropogenic activities can significantly cause the climate change. At the same time, the change in the total net radiation depends on the geophysical conditions This study provides estimates of the anthropogenic forcing of the most important greenhouse gases (carbon dioxide (CO2), ozone (O3)), as well as atmospheric aerosol on atmospheric radiation (RF) in the SW and LW spectrum. We determined the features of the vertical profiles of RF and their values at the bottom (BOA) and at the top of the atmosphere (TOA) depending solar elevation and surface albedo, taking into account for seasonal variations. Estimates of their radiative forcing were calculated for the Moscow region using the ECRAD model