Gravitační pole Měsíce a jeho "aspekty"

Abstract

By utilizing the Moon's satellite missions and lunar gravity models, it is not possible only to know the Moon's surface, but also the distribution of mass and bark thickness. The result is a set of Stokes parameters, from which the "aspects" of geopotential are calculated to determine the geophysical properties of a surface. The display of these aspects makes it possible to know not only the surface, but also what has been hidden under it for many years.