Changes in the solar constant and the dynamics of global air temperatures in the surface layer of the atmosphere in the late Pleistocene – Holocene
Changes in the medieval values of global surface air temperatures in the Late Pleistocene-Holocene were due changes phases Milankovich cycles and Patterson-Shnitnikov generating the dynamics of average annual values of the solar constant and the evolution of the planet's cryosphere, that alters the distribution of the surface albedo.