Аннотация:The explicit form for the quadratic contribution to the gravitational field from the dipole distributed
anomalous masses is found. The anomalous masses are represented in the form of layers of variable
height, arranged relative to the reference ellipsoid. The solution is reduced to the mathematical problem
of finding an expression for the coefficients of expansion in terms of spherical harmonics of the square of
any function that can be presented as a finite series of spherical harmonics, in terms of the coefficients
of this initial series. The formulas have been calculated using mathematical modelling of symbol
computation using computer algebra packages. The results obtained are illustrated using the example
of the contribution from relief masses and density jumps on the Mohorovicic (Moho) discontinuity