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提出内蕴大地边值问题,使得有可能利用重力场边界观测研究地球重力场的内蕴结构。文中构造了椭球问题的迭代逼近求解程式,并给出了具体解式。
Proposing the problem of intrinsic geodetic boundary value makes it possible to use the boundary of the gravity field to observe and study the intrinsic structure of the Earth's gravitational field. In this paper, an iterative approximation solution to the ellipsoid problem is constructed, and a concrete solution is given.